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r276 r277 7 7 timestamp={20121015}, 8 8 hal_id = {hal-00023597}, 9 title = {{La s {\'e}dimentation organo-min{\'e}rale marqueur des changements environnementaux et climatiques au Nord-Est du Br{\'e}sil (Lac Ca{\c c}o, Maranh{\\~a}o, Br{\'e}sil) durant les 21,000 ans Cal BP.}},10 author = { Abdelfettah Sifeddine and Ana Luiza Spadano Albuquerque and Bruno Turcq and Jérémy Jacob and Mohammed Boussafir and Jean-Robert Disnar and Jorge Abrão},11 abstract = {{Les r {\'e}sultats s{\'e}dimentologiques incluant la sismique r{\'e}flexion, la min{\'e}ralogie et la g{\'e}ochimie organique de deux carottes pr{\'e}lev{\'e}es respectivement au centre et sur la marge du lac Ca{\c c}o- (Maranh{\\~a}o,Br{\'e}sil) ont mit en {\'e}vidence des changement climatiques et environnementaux durant les 21 000 derni{\`e}res ann{\'e}es. En g{\'e}n{\'e}ral le Tardi glaciaire a {\'e}t{\'e} marqu{\'e} par trois phases d'augmentation du niveau du lac dat{\'e}es respectivement vers 17,400; 14,900 et 12,000 ans Cal B.P. accompagn{\'e}es chaque fois par des pics de Sid{\'e}rite. Le Dryas r{\'e}cent a {\'e}t{\'e} enregistr{\'e} au lac Ca{\c c}o par une diminution du niveau lacustre. Compar{\'e}s avec d'autres enregistrements pal{\'e}oclimatiques d'Am{\'e}rique du Sud, il appara{\^\i}t que le climat r{\'e}gional du lac Ca{\c c}o a {\'e}t{\'e} principalement contr{\^o}l{\'e} par des {\'e}v{\'e}nements globaux ainsi que par les interconnections entre les deux h{\'e}misph{\`e}res. L'Holoc{\`e}ne, a {\'e}t{\'e} marqu{\'e} entre 10,000 et 7,000 ans Cal B.P. par un arr{\^e}t de la s{\'e}dimentation dans la marge du lac (MA 97-3). La pr{\'e}sence de charbons de bois {\`a} partir 10,000 ans B.P., confirme l'existence de phases s{\`e}ches durant cette p{\'e}riode. A partir de 7,000 ans Cal B.P., le lac Ca{\c c}o enregistre une nouvelle phase de remise en eau.}},12 language = { Anglais},13 affiliation = { Departamento de Geoquimica, Universidade Federal Fluminense - DEPARTAMENTO DE GEOQUIMICA , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO},14 booktitle = {{Association des S{\'e}dimentologistes Fran{\c c}ais}},15 address = { Orl{\'e}ans, France},9 title = {{La sédimentation organo-minérale marqueur des changements environnementaux et climatiques au {N}ord-{E}st du {B}résil (Lac {C}aço, {M}aranhão, {B}résil) durant les 21,000 ans {C}al BP.}}, 10 author = {{A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq and {J}érémy {J}acob and {M}ohammed {B}oussafir and {J}ean-{R}obert {D}isnar and {J}orge {A}brão}, 11 abstract = {{Les résultats sédimentologiques incluant la sismique réflexion, la minéralogie et la géochimie organique de deux carottes prélevées respectivement au centre et sur la marge du lac {C}aço- (Maranhão,Brésil) ont mit en évidence des changement climatiques et environnementaux durant les 21 000 dernières années. {E}n général le {T}ardi glaciaire a été marqué par trois phases d'augmentation du niveau du lac datées respectivement vers 17,400; 14,900 et 12,000 ans {C}al B.P. accompagnées chaque fois par des pics de {S}idérite. {L}e {D}ryas récent a été enregistré au lac {C}aço par une diminution du niveau lacustre. {C}omparés avec d'autres enregistrements paléoclimatiques d'{A}mérique du {S}ud, il apparaît que le climat régional du lac {C}aço a été principalement contrôlé par des événements globaux ainsi que par les interconnections entre les deux hémisphères. L'{H}olocène, a été marqué entre 10,000 et 7,000 ans {C}al B.P. par un arrêt de la sédimentation dans la marge du lac (MA 97-3). {L}a présence de charbons de bois à partir 10,000 ans B.P., confirme l'existence de phases sèches durant cette période. A partir de 7,000 ans {C}al B.P., le lac {C}aço enregistre une nouvelle phase de remise en eau.}}, 12 language = {{A}nglais}, 13 affiliation = {{D}epartamento de {G}eoquimica, {U}niversidade {F}ederal {F}luminense - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO}, 14 booktitle = {{Association des {S}édimentologistes {F}rançais}}, 15 address = {{O}rléans, {F}rance}, 16 16 year = {2001}, 17 17 } … … 21 21 loceanbibid = {01910}, 22 22 timestamp={20121115}, 23 title = {{Enregistrement des variations pal {\'e}oenvironnementales durant le Quaternaire r{\'e}cent en domaine intertropical (Lac Ca{\c c}o, Br{\'e}sil) : Apports de la g{\'e}ochimie organique globale et mol{\'e}culaire.}},24 author = { Jérémy Jacob and Jean-Robert Disnar and Mohammed Boussafir and Abdelfettah Sifeddine and Ana-Luiza Spadano Albuquerque and Bruno Turcq},25 language = { Fran{\c c}ais},26 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Departamento de Geoquimica, Universidade Federal Fluminense - DEPARTAMENTO DE GEOQUIMICA , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},27 booktitle = {{Association des S{\'e}dimentologiqtes Fran{\c c}ais}},28 address = { Orl{\'e}ans, France},23 title = {{Enregistrement des variations paléoenvironnementales durant le {Q}uaternaire récent en domaine intertropical (Lac {C}aço, {B}résil) : {A}pports de la géochimie organique globale et moléculaire.}}, 24 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir and {A}bdelfettah {S}ifeddine and {A}na-{L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 25 language = {{F}rançais}, 26 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {D}epartamento de {G}eoquimica, {U}niversidade {F}ederal {F}luminense - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 27 booktitle = {{Association des {S}édimentologiqtes {F}rançais}}, 28 address = {{O}rléans, {F}rance}, 29 29 year = {2001}, 30 30 pdf = {http://hal-insu.archives-ouvertes.fr/hal-00022464/PDF/13\_-\_Resume\_Lac\_Caco\_-\_ASF-Oral\_-\_Jacob\_et\_al\_2001.pdf}, … … 35 35 loceanbibid = {01909}, 36 36 timestamp={20121115}, 37 title = {{Onocerane I witnesses to dry climatic phases at the end of Last Glacial Maximum and during the Younger Dryas in Northern Brazil.}},38 author = { Jérémy Jacob and Jean-Robert Disnar and Mohammed Boussafir and Marie-Pierre Ledru and Abdelfettah Sifeddine and Ana Luiza Spadano Albuquerque and Bruno Turcq},39 abstract = {{Onocerane-related compounds are very uncommon molecules that are seldom encountered in the plant kingdom and even more rarely in sediments. In living plants, onoceranoids have been isolated from taxa as diverse as ferns, club mosses and Fabaceae. In this latter, onocerin (onoceranediol) is supposed to render the roots water-impermeable and to allow the plants belonging to this genus to colonize water-depleted media. In sediments, onoceranes have been observed up to the Carboniferous but mainly in post-Cretaceous series always deposited in continental settings (lacustrine, intramontane basins, lagoonal or brackish contexts). We here report on the first occurrence of onocerane I in Late Pleistocene and Quaternary sediments, collected in a lake located almost under the Equator (Lagoa do Ca{\c c}o, NE Brazil). The comparison of onocerane I abundance with palynological results all through the last 20,000 years allow us to exclude ferns and club mosses as possible producers of onocerane in this setting. Onocerane I is only found in significant amounts in two distinct sedimentary intervals: the first, rapidly deposited at the end of Last Glacial Maximum (c.a. 21,000 cal yrs B.P.) and the second during the Younger Dryas (between 13,000 and 12,000 cal yrs B.P.) (figure 1). These two periods are both documented as having been dryer than those prevailing presently. Therefore, the presence of onocerane I in the sediments deposited during these two intervals testimonies to the development of plants adapted to water-deficient environments. No evidence of a possible precursor can be deciphered from palynological results, probably due to the poor conservation of the pollen of these plants.}},40 language = { Anglais},41 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Departamento Geologia Sedimentar e Ambiental - IRD/CNPQ , Departamento de Geoquimica, Universidade Federal Fluminense - DEPARTAMENTO DE GEOQUIMICA , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},42 booktitle = {{21st International Meeting on Organic Geochemistry}},43 address = { Kralow, Pologne},37 title = {{Onocerane I witnesses to dry climatic phases at the end of {L}ast {G}lacial {M}aximum and during the {Y}ounger {D}ryas in {N}orthern {B}razil.}}, 38 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir and {M}arie-{P}ierre {L}edru and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 39 abstract = {{Onocerane-related compounds are very uncommon molecules that are seldom encountered in the plant kingdom and even more rarely in sediments. {I}n living plants, onoceranoids have been isolated from taxa as diverse as ferns, club mosses and {F}abaceae. {I}n this latter, onocerin (onoceranediol) is supposed to render the roots water-impermeable and to allow the plants belonging to this genus to colonize water-depleted media. {I}n sediments, onoceranes have been observed up to the {C}arboniferous but mainly in post-{C}retaceous series always deposited in continental settings (lacustrine, intramontane basins, lagoonal or brackish contexts). {W}e here report on the first occurrence of onocerane I in {L}ate {P}leistocene and {Q}uaternary sediments, collected in a lake located almost under the {E}quator (Lagoa do {C}aço, NE {B}razil). {T}he comparison of onocerane I abundance with palynological results all through the last 20,000 years allow us to exclude ferns and club mosses as possible producers of onocerane in this setting. {O}nocerane I is only found in significant amounts in two distinct sedimentary intervals: the first, rapidly deposited at the end of {L}ast {G}lacial {M}aximum (c.a. 21,000 cal yrs B.P.) and the second during the {Y}ounger {D}ryas (between 13,000 and 12,000 cal yrs B.P.) (figure 1). {T}hese two periods are both documented as having been dryer than those prevailing presently. {T}herefore, the presence of onocerane I in the sediments deposited during these two intervals testimonies to the development of plants adapted to water-deficient environments. {N}o evidence of a possible precursor can be deciphered from palynological results, probably due to the poor conservation of the pollen of these plants.}}, 40 language = {{A}nglais}, 41 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {D}epartamento {G}eologia {S}edimentar e {A}mbiental - IRD/CNPQ , {D}epartamento de {G}eoquimica, {U}niversidade {F}ederal {F}luminense - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 42 booktitle = {{21st {I}nternational {M}eeting on {O}rganic {G}eochemistry}}, 43 address = {{K}ralow, {P}ologne}, 44 44 year = {2003}, 45 45 pdf = {http://hal-insu.archives-ouvertes.fr/hal-00022465/PDF/16-\_Resume\_Onocerane\_-\_IMOG-Oral\_-\_Jacob\_et\_al\_2003.pdf}, … … 51 51 timestamp={20121115}, 52 52 url = {http://hal-insu.archives-ouvertes.fr/hal-00085104}, 53 title = {{Distribution et {\'e}tat de pr{\'e}servation de la mati{\`e}re organique s{\'e}dimentaire des s{\'e}diments superficiels du Lac Ca{\c c}o (Maran{\\~a}o, Br{\'e}sil). Production/diagen{\`e}se organique pr{\'e}coce et remplissage s{\'e}dimentaire lacustre}},54 author = { Mohammed Boussafir and Merouane Foudi and Jérémy Jacob and Jean-Robert Disnar and Abdelfettah Sifeddine and Ana Luiza Spadano Albuquerque},55 abstract = {{Le Lac Ca{\c c}o est situ{\'e} au Nord-Est du Br{\'e}sil, dans l'Etat de Maranha{\\~o}, sous l'Equateur (2°58S 43°25 W), en bordure de la for{\^e}t amazonienne et {\`a} 80 km de la c{\^o}te Atlantique. Son altitude ne d{\'e}passe pas les 80m. Ce lac est largement influenc{\'e} par le climat intertropical humide (1500 {\`a} 1750mm/an), caract{\'e}ris{\'e} par une saison pluvieuse de 6 mois, de d{\'e}cembre jusqu'au mois de mai. La temp{\'e}rature annuelle moyenne est de 26°C. Sa situation {\`a} l'entr{\'e}e de le zone de convergence intertropicale lui conf{\`e}re une importance majeure dans les {\'e}tudes pal{\'e}oenvironnementales et pal{\'e}oclimatiques quaternaires du continent sud am{\'e}ricain. L'objectif principal de ce travail {\'e}tait d'{\'e}tudier la nature, l'{\'e}tat de pr{\'e}servation et les sources actuelles de la MO s{\'e}dimentaire d'un bassin lacustre {\'e}quatorial, par le moyen d'analyses globales en g{\'e}ochimie et p{\'e}trographie organiques.}},56 language = { Anglais},57 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Departamento de Geoquimica - DEPARTAMENTO DE GEOQUIMICA},58 booktitle = {{Association des S{\'e}dimentologistes Fran{\c c}ais}},59 address = { Bordeaux, France},53 title = {{Distribution et état de préservation de la matière organique sédimentaire des sédiments superficiels du {L}ac {C}aço (Maranhaão, {B}résil). {P}roduction/diagenèse organique précoce et remplissage sédimentaire lacustre}}, 54 author = {{M}ohammed {B}oussafir and {M}erouane {F}oudi and {J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque}, 55 abstract = {{Le {L}ac {C}aço est situé au {N}ord-{E}st du {B}résil, dans l'{E}tat de {M}aranhaõ}, sous l'{E}quateur (2°58S 43°25 W), en bordure de la forêt amazonienne et à 80 km de la côte {A}tlantique. {S}on altitude ne dépasse pas les 80m. {C}e lac est largement influencé par le climat intertropical humide (1500 à 1750mm/an), caractérisé par une saison pluvieuse de 6 mois, de décembre jusqu'au mois de mai. {L}a température annuelle moyenne est de 26°C. {S}a situation à l'entrée de le zone de convergence intertropicale lui confère une importance majeure dans les études paléoenvironnementales et paléoclimatiques quaternaires du continent sud américain. L'objectif principal de ce travail était d'étudier la nature, l'état de préservation et les sources actuelles de la MO sédimentaire d'un bassin lacustre équatorial, par le moyen d'analyses globales en géochimie et pétrographie organiques.}}, 56 language = {{A}nglais}, 57 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA}, 58 booktitle = {{Association des {S}édimentologistes {F}rançais}}, 59 address = {{B}ordeaux, {F}rance}, 60 60 year = {2003}, 61 61 pdf = {http://hal-insu.archives-ouvertes.fr/hal-00085104/PDF/17\_-\_Resume\_-ASF-poster\_-\_Boussafiretal2003.pdf}, … … 66 66 loceanbibid = {01907}, 67 67 timestamp={20121115}, 68 title = {{Mg- Calcites and dolomite in the Brejo do Espinho lagoon, Rio de Janeiro.}},69 author = {A.P.A. Anjos and Abdelfettah Sifeddine and S.R. Pachineelam and Christian Défarge and Bruno Turcq},70 abstract = {{The aim of this research is to study the carbonate sedimentation in a hypersaline coastal (Brejo do Espinho) where dolomite precipitation can be expected. The study allowed to make a general characterization of the sediment and to identify different types of carbonate minerals by mineralogical studies and cryo-scanning electron-microscopy.}},71 language = { Anglais},72 affiliation = { Departamento de Geoquimica Universidade Federal Fluminense, Morro do Valonguinho - DEPARTAMENTO DE GEOQUIMICA , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO},73 booktitle = {{3rd Latin American Congr. Sedimentology}},74 address = { Bel{\'e}m, Br{\'e}sil},68 title = {{Mg-{C}alcites and dolomite in the {B}rejo do {E}spinho lagoon, {R}io de {J}aneiro.}}, 69 author = {A.P.A. {A}njos and {A}bdelfettah {S}ifeddine and S.R. {P}achineelam and {C}hristian {D}éfarge and {B}runo {T}urcq}, 70 abstract = {{The aim of this research is to study the carbonate sedimentation in a hypersaline coastal (Brejo do {E}spinho) where dolomite precipitation can be expected. {T}he study allowed to make a general characterization of the sediment and to identify different types of carbonate minerals by mineralogical studies and cryo-scanning electron-microscopy.}}, 71 language = {{A}nglais}, 72 affiliation = {{D}epartamento de {G}eoquimica {U}niversidade {F}ederal {F}luminense, {M}orro do {V}alonguinho - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO}, 73 booktitle = {{3rd {L}atin {A}merican {C}ongr. {S}edimentology}}, 74 address = {{B}elém, {B}résil}, 75 75 year = {2003}, 76 76 pdf = {http://hal-insu.archives-ouvertes.fr/hal-00089101/PDF/CDCc30.pdf}, … … 81 81 loceanbibid = {01906}, 82 82 timestamp={20121115}, 83 title = {{Reconstruction of pAST climates from sedimentary biomarkers. Ancient molecules for past climate reconstructions: a large field of application for spectroscopic methods.}},84 author = { Jérémy Jacob and Jean-Robert Disnar and Yongsong Huang and Mohammed Boussafir and Abdelfettah Sifeddine and Ana Luiza Spadano Albuquerque and Bruno Turcq},85 abstract = {{Although we have now a better picture of past climates, there are still numerous questions that remain unsolved. These uncertainties primarily arise from the possible human impact on climate dynamics, the need to assess feedbacks from the biosphere and to better understand and anticipate natural variability of climate (forcing mechanisms, time lags...). In order to record past climatic and environmental changes, numerous tools have been applied to multiple records. The direct interpretation of these data in terms of climatic parameters is sometimes questionable and strengthens the necessity for more accurate paleodata from sedimentary archives. Sedimentary organic matter is a renewing target for paleoclimate information because it derives from living organisms that are sensible to environmental changes and its complexity promises a virtually infinite source of information. In order to access this information at a molecular or isotopic level, the organic geochemist must now use a large panel of spectroscopic tools (GC-MS, HPLC-MS and GC-IRMS). I will here present some recent advances in the field of molecular and compound-specific isotopes applications to paleoclimate reconstructions. So as to estimate the impact of climatic changes on the ecosystems, paleoflora can be deciphered from the occurrence, in the sediments, of taxon-specific molecules. Similarly, the physico-chemical conditions that prevailed at time of deposition of the sediment are accessible by the study of diagenetic by-products, derived from the alteration of biomolecules. Other molecules are produced by organisms as a response to the variations of environmental/climatic parameters. Their identification and quantitation in sediments can be used as a proxy of these parameters. Finally, the recent development of compound-specific isotope techniques allows measuring the isotopic composition ($\Delta$D, $\Delta$13C, 15N...) of single molecules, therefore affording a better constrain on the significance of isotopic signatures.}},86 language = { Anglais},87 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Geology Department , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Departamento de Geoquimica, Universidade Federal Fluminense - DEPARTAMENTO DE GEOQUIMICA},88 booktitle = {{21 {\`e}me Congr{\`e}s de la Soci{\'e}t{\'e} Fran{\c c}aise de Spectrom{\'e}trie de Masse}},89 address = { Strasbourg, France},83 title = {{Reconstruction of pAST climates from sedimentary biomarkers. {A}ncient molecules for past climate reconstructions: a large field of application for spectroscopic methods.}}, 84 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {Y}ongsong {H}uang and {M}ohammed {B}oussafir and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 85 abstract = {{Although we have now a better picture of past climates, there are still numerous questions that remain unsolved. {T}hese uncertainties primarily arise from the possible human impact on climate dynamics, the need to assess feedbacks from the biosphere and to better understand and anticipate natural variability of climate (forcing mechanisms, time lags...). {I}n order to record past climatic and environmental changes, numerous tools have been applied to multiple records. {T}he direct interpretation of these data in terms of climatic parameters is sometimes questionable and strengthens the necessity for more accurate paleodata from sedimentary archives. {S}edimentary organic matter is a renewing target for paleoclimate information because it derives from living organisms that are sensible to environmental changes and its complexity promises a virtually infinite source of information. {I}n order to access this information at a molecular or isotopic level, the organic geochemist must now use a large panel of spectroscopic tools (GC-MS, HPLC-MS and GC-IRMS). I will here present some recent advances in the field of molecular and compound-specific isotopes applications to paleoclimate reconstructions. {S}o as to estimate the impact of climatic changes on the ecosystems, paleoflora can be deciphered from the occurrence, in the sediments, of taxon-specific molecules. {S}imilarly, the physico-chemical conditions that prevailed at time of deposition of the sediment are accessible by the study of diagenetic by-products, derived from the alteration of biomolecules. {O}ther molecules are produced by organisms as a response to the variations of environmental/climatic parameters. {T}heir identification and quantitation in sediments can be used as a proxy of these parameters. {F}inally, the recent development of compound-specific isotope techniques allows measuring the isotopic composition ($\Delta$D, $\Delta$13C, 15N...) of single molecules, therefore affording a better constrain on the significance of isotopic signatures.}}, 86 language = {{A}nglais}, 87 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {G}eology {D}epartment , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {D}epartamento de {G}eoquimica, {U}niversidade {F}ederal {F}luminense - DEPARTAMENTO DE GEOQUIMICA}, 88 booktitle = {{21ème {C}ongrès de la {S}ociété {F}rançaise de {S}pectrométrie de {M}asse}}, 89 address = {{S}trasbourg, {F}rance}, 90 90 year = {2004}, 91 91 } … … 95 95 loceanbibid = {01905}, 96 96 timestamp={20121115}, 97 title = {{Agricultura y medio natural en la cuenca del Titicaca : tres mil anos de relaciones}},98 author = { Thérèse Bouysse-Cassagne and P. Morlon and Philippe Mourguiart and Denis Wirrmann},99 keywords = { Exploitation agricole;histoire;utilisation du sol;Andes;Bolivie;P{\'e}rou;Lac Titicaca},100 language = { Espagnol},101 affiliation = { Centre de recherche et de documentation de l'Am{\'e}rique latine - CREDAL , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},97 title = {{Agricultura y medio natural en la cuenca del {T}iticaca : tres mil anos de relaciones}}, 98 author = {{T}hérèse {B}ouysse-{C}assagne and P. {M}orlon and {P}hilippe {M}ourguiart and {D}enis {W}irrmann}, 99 keywords = {{E}xploitation agricole;histoire;utilisation du sol;Andes;Bolivie;Pérou;Lac {T}iticaca}, 100 language = {{E}spagnol}, 101 affiliation = {{C}entre de recherche et de documentation de l'{A}mérique latine - CREDAL , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 102 102 booktitle = {{Actas del septimo congreso internacional sobre cultivos andinos}}, 103 103 publisher = {ORSTOM ; IBTA ; CRDI}, 104 104 pages = {383-389}, 105 address = { La Paz, Bolivie, L'{\'E}tat Plurinational De},105 address = {{L}a {P}az, {B}olivie, L'État {P}lurinational {D}e}, 106 106 volume = {7}, 107 editor = { Morales D., Vacher Jean (eds.)},108 note = { Disponible en ligne sur : http://horizon.documentation.ird.fr/exl-doc/pleins\_textes/divers09-11/38559.pdf},107 editor = {{M}orales D., {V}acher {J}ean (eds.)}, 108 note = {{D}isponible en ligne sur : http://horizon.documentation.ird.fr/exl-doc/pleins\_textes/divers09-11/38559.pdf}, 109 109 audience = {internationale}, 110 110 year = {1992}, … … 115 115 loceanbibid = {01905}, 116 116 timestamp={20121115}, 117 title = {{Nouveaux marqueurs mol {\'e}culaires t{\'e}moins des successions v{\'e}g{\'e}tales en domaine tropical. Exemple du Lac Ca{\c c}{\'o} (Nord Est Br{\'e}sil) depuis le DMG.}},118 author = { Jérémy Jacob and Jean-Robert Disnar and Mohammed Boussafir and Abdelfettah Sifeddine and Ana Luiza Spadano Albuquerque and Bruno Turcq},119 abstract = {{La reconstitution des climats anciens n {\'e}cessite soit un acc{\`e}s direct aux param{\`e}tres qui les d{\'e}finissent (temp{\'e}rature, humidit{\'e}...) soit, de fa{\c c}on indirecte, aux environnements et {\'e}cosyst{\`e}mes qui se sont d{\'e}velopp{\'e}s sous ces climats. En domaine continental, ces {\'e}cosyst{\`e}mes sont principalement caract{\'e}ris{\'e}s par des associations v{\'e}g{\'e}tales que la palynologie et d'autres outils tels que les isotopes du carbone permettent en partie de reconstituer. Notre approche, compl{\'e}mentaire de la palynologie, est fond{\'e}e sur l'identification de biomarqueurs organiques, c'est-{\`a}-dire de mol{\'e}cules qui se sont pr{\'e}serv{\'e}es dans les s{\'e}diments et dont la structure permet d'{\'e}tablir une relation directe avec le groupe d'organismes les ayant produites, ce groupe {\'e}tant le plus restreint possible.}},120 language = { Fran{\c c}ais},121 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Departamento de Geoquimica - DEPARTAMENTO DE GEOQUIMICA},122 booktitle = {{Association des S{\'e}dimentologistes Fran{\c c}ais}},117 title = {{Nouveaux marqueurs moléculaires témoins des successions végétales en domaine tropical. {E}xemple du {L}ac {C}açó (Nord {E}st {B}résil) depuis le DMG.}}, 118 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 119 abstract = {{La reconstitution des climats anciens nécessite soit un accès direct aux paramètres qui les définissent (température, humidité...) soit, de façon indirecte, aux environnements et écosystèmes qui se sont développés sous ces climats. {E}n domaine continental, ces écosystèmes sont principalement caractérisés par des associations végétales que la palynologie et d'autres outils tels que les isotopes du carbone permettent en partie de reconstituer. {N}otre approche, complémentaire de la palynologie, est fondée sur l'identification de biomarqueurs organiques, c'est-à-dire de molécules qui se sont préservées dans les sédiments et dont la structure permet d'établir une relation directe avec le groupe d'organismes les ayant produites, ce groupe étant le plus restreint possible.}}, 120 language = {{F}rançais}, 121 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA}, 122 booktitle = {{Association des {S}édimentologistes {F}rançais}}, 123 123 pages = {3 p.}, 124 address = { Bordeaux, France},124 address = {{B}ordeaux, {F}rance}, 125 125 editor = {ASF}, 126 126 audience = {nationale}, … … 134 134 loceanbibid = {01904}, 135 135 timestamp={20121115}, 136 title = {{Sensibilite de la sedimentation organique aux variations climatiques du Tardi-Wuerm et de l'Holocene; le lac du Bouchet (Haute-Loire, France)}},137 author = { Elisabeth Lallier-Vergès and Abdelfettah Sifeddine and Jacques Louis De Beaulieu and Maurice Reille and Nicolas Tribovillard and Philippe Bertrand and Thierry Mongenot and Nicolas Thouveny and Jean-Robert Disnar and Bernard Guillet},138 abstract = {{Deux carottes de s {\'e}diments superficiels (2 {\`a} 3 m) pr{\'e}lev{\'e}es dans le lac du Bouchet (Haute Loire, France) ont {\'e}t{\'e} {\'e}tudi{\'e}es du point de vue de leur composition min{\'e}rale et organique. Les corr{\'e}lations {\'e}tablies {\`a} partir des donn{\'e}es concernant lamati{\`e}re organique ainsi que celles de la palynologie, ont permis de replacer les deux premiers m{\`e}tres de la s{\'e}rie s{\'e}dimentaire dans la logique climato-stratigraphique du passage Tardi-W{\"u}rm-Holoc{\`e}ne. Nous montrons ici que des variations climatiques de faible amplitude comme celles de l'Holoc{\`e}ne, engendrent des changements importants dans la nature, la quantit{\'e} et le mode de pr{\'e}servation des constituants organiques s{\'e}diment{\'e}s.}},139 keywords = { Lac de maar, Lac du Bouchet, S{\'e}dimentation organo-min{\'e}rale, Palynofaci{\`e}s, Palynologie, Tardi-W{\"u}rm, Holoc{\`e}ne},140 language = { Fran{\c c}ais},141 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Laboratoire de chrono-{\'e}cologie - LCE , Institut M{\'e}diterran{\'e}en d'Ecologie et de Pal{\'e}o{\'e}cologie - IMEP , Processus et bilan des domaines s{\'e}dimentaires - PBDS , Environnements et Pal{\'e}oenvironnements OC{\'e}aniques - EPOC},136 title = {{Sensibilite de la sedimentation organique aux variations climatiques du {T}ardi-{W}uerm et de l'{H}olocene; le lac du {B}ouchet (Haute-{L}oire, {F}rance)}}, 137 author = {{E}lisabeth {L}allier-{V}ergès and {A}bdelfettah {S}ifeddine and {J}acques {L}ouis {D}e {B}eaulieu and {M}aurice {R}eille and {N}icolas {T}ribovillard and {P}hilippe {B}ertrand and {T}hierry {M}ongenot and {N}icolas {T}houveny and {J}ean-{R}obert {D}isnar and {B}ernard {G}uillet}, 138 abstract = {{Deux carottes de sédiments superficiels (2 à 3 m) prélevées dans le lac du {B}ouchet (Haute {L}oire, {F}rance) ont été étudiées du point de vue de leur composition minérale et organique. {L}es corrélations établies à partir des données concernant lamatière organique ainsi que celles de la palynologie, ont permis de replacer les deux premiers mètres de la série sédimentaire dans la logique climato-stratigraphique du passage {T}ardi-{W}ürm-{H}olocène. {N}ous montrons ici que des variations climatiques de faible amplitude comme celles de l'{H}olocène, engendrent des changements importants dans la nature, la quantité et le mode de préservation des constituants organiques sédimentés.}}, 139 keywords = {{L}ac de maar, {L}ac du {B}ouchet, {S}édimentation organo-minérale, {P}alynofaciès, {P}alynologie, {T}ardi-{W}ürm, {H}olocène}, 140 language = {{F}rançais}, 141 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {L}aboratoire de chrono-écologie - LCE , {I}nstitut {M}éditerranéen d'{E}cologie et de {P}aléoécologie - IMEP , {P}rocessus et bilan des domaines sédimentaires - PBDS , {E}nvironnements et {P}aléoenvironnements OCéaniques - EPOC}, 142 142 pages = {5, 661-673}, 143 journal = { Bulletin de la Soci{\'e}t{\'e} G{\'e}ologique de France},143 journal = {{B}ulletin de la {S}ociété {G}éologique de {F}rance}, 144 144 volume = {164}, 145 audience = {non sp {\'e}cifi{\'e}e},145 audience = {non spécifiée}, 146 146 year = {1993}, 147 147 pdf = {http://hal-insu.archives-ouvertes.fr/hal-00122515/PDF/010022542.pdf}, … … 152 152 loceanbibid = {01903}, 153 153 timestamp={20121115}, 154 title = {{A 36 ka environmental record in the southern tropics : Lake Tritrivakely (Madgascar) (Un enregistrement de l'environnement depuis 36 ka en zone tropicale sud : le lac Tritrivakely (Madagascar)).}},155 author = { Françoise Gasse and Elsa Cortijo and Jean-Robert Disnar and Luc Ferry and Elisabeth Gilbert and Catherine Kissel and Fatima Laggoun-Défarge and Elisabeth Lallier-Vergès and Jean-Claude Miskovsky and Bruno Ratsimbazafy and Flavien Ranaivo and Laurent Robinson and Piotr Tucholka and Jean-Luc Saos and Abdelfettah Sifeddine and Maurice Taieb and Elise Van Campo and David Williamson},156 abstract = {{The upper 13 m of a 40 m-long sedimentary profile core taken in a crater lake on the Malagasy Plateau reveals 36,000 yrs of hydroclimatic evolution. A shallow lake occupies the core site from 35 to 19 ka BP under climatic conditions cooler than today. The water table is very low and biological productivity extremely reduced during the Last Glacial Maximum. A large warming was initiated at 14.5 ka BP. The modern bog establishes about 4 ka ago}},157 keywords = { Malagasy Republic ; lake sediments ; cores ; drilling ; paleoenvironment ; paleoclimatology ; paleotemperature ; paleohydrology ; warming ; peat bogs ; tropical environment ; upper Quaternary ; absolute age ; C-14 ; stable isotopes ; C-13 ; Indian Ocean Islands},158 language = { Anglais},159 affiliation = { Centre europ{\'e}en de recherche et d'enseignement de g{\'e}osciences de l'environnement - CEREGE , CNRS - ORSTOM Pal{\'e}ohydrologie, Pal{\'e}oclimatique Continentales , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Laboratoire des sciences du climat et de l'environnement - LSCE , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},154 title = {{A 36 ka environmental record in the southern tropics : {L}ake {T}ritrivakely (Madgascar) (Un enregistrement de l'environnement depuis 36 ka en zone tropicale sud : le lac {T}ritrivakely (Madagascar)).}}, 155 author = {{F}rançoise {G}asse and {E}lsa {C}ortijo and {J}ean-{R}obert {D}isnar and {L}uc {F}erry and {E}lisabeth {G}ilbert and {C}atherine {K}issel and {F}atima {L}aggoun-{D}éfarge and {E}lisabeth {L}allier-{V}ergès and {J}ean-{C}laude {M}iskovsky and {B}runo {R}atsimbazafy and {F}lavien {R}anaivo and {L}aurent {R}obinson and {P}iotr {T}ucholka and {J}ean-{L}uc {S}aos and {A}bdelfettah {S}ifeddine and {M}aurice {T}aieb and {E}lise {V}an {C}ampo and {D}avid {W}illiamson}, 156 abstract = {{The upper 13 m of a 40 m-long sedimentary profile core taken in a crater lake on the {M}alagasy {P}lateau reveals 36,000 yrs of hydroclimatic evolution. A shallow lake occupies the core site from 35 to 19 ka BP under climatic conditions cooler than today. {T}he water table is very low and biological productivity extremely reduced during the {L}ast {G}lacial {M}aximum. A large warming was initiated at 14.5 ka BP. {T}he modern bog establishes about 4 ka ago}}, 157 keywords = {{M}alagasy {R}epublic ; lake sediments ; cores ; drilling ; paleoenvironment ; paleoclimatology ; paleotemperature ; paleohydrology ; warming ; peat bogs ; tropical environment ; upper {Q}uaternary ; absolute age ; C-14 ; stable isotopes ; C-13 ; {I}ndian {O}cean {I}slands}, 158 language = {{A}nglais}, 159 affiliation = {{C}entre européen de recherche et d'enseignement de géosciences de l'environnement - CEREGE , CNRS - ORSTOM {P}aléohydrologie, {P}aléoclimatique {C}ontinentales , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {L}aboratoire des sciences du climat et de l'environnement - LSCE , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 160 160 pages = {1513-1519}, 161 journal = { Comptes Rendus de l'Acad{\'e}mie des Sciences - Series IIA - Earth and Planetary Science},161 journal = {{C}omptes {R}endus de l'{A}cadémie des {S}ciences - {S}eries IIA - {E}arth and {P}lanetary {S}cience}, 162 162 volume = {318}, 163 note = {GDR 970 : CNRS - ORSTOM Pal{\'e}ohydrologie, Pal{\'e}oclimatique Continentales},164 audience = {non sp {\'e}cifi{\'e}e},163 note = {GDR 970 : CNRS - ORSTOM {P}aléohydrologie, {P}aléoclimatique {C}ontinentales}, 164 audience = {non spécifiée}, 165 165 year = {1994}, 166 166 pdf = {http://hal-insu.archives-ouvertes.fr/hal-00122534/PDF/42480.pdf}, 167 167 } 168 168 169 @article{SifeddineLaggoun -DefargeEtAl:AS:1995,169 @article{SifeddineLaggoundefargeEtAl:AS:1995, 170 170 hal_id = {hal-00068937}, 171 171 loceanbibid = {01902}, 172 172 timestamp={20121115}, 173 173 url = {http://hal-insu.archives-ouvertes.fr/hal-00068937}, 174 title = {{L a s{\'e}dimentation organique lacustre en zone tropicale sud au cours des 36 O00 derni{\`e}res ann{\'e}es (Lac Tritrivakely, Madagascar).}},175 author = { Abdelfettah Sifeddine and Fatima Laggoun-Défarge and Elisabeth Lallier-Vergès and Jean-Robert Disnar and David Williamson and Françoise Gasse and Elisabeth Gibert},176 abstract = {{L' {\'e}tude p{\'e}trographique (palynofaci{\`e}s) et g{\'e}ochimique (pyrolyse Rock Eval) de la mati{\`e}re organique s{\'e}dimentaire d'une carotte pr{\'e}lev{\'e}e dans un lac de crat{\`e}re de Madagascar r{\'e}v{\`e}le une s{\'e}dimentation organique de type tourbeux avant 36 ka, entre ca 28 et 15 ka et entre 6 et O ka, mise en place au cours de p{\'e}riodes d'ass{\'e}chement. Entre ca 36 et 28 ka, elle se caract{\'e}rise par une s{\'e}dimentation lacustre (phytoplancton dominant) et des migrations de v{\'e}g{\'e}tation du bassin versant vers le lac luim{\^e}me. Des apports de mati{\`e}re organique allochtone t{\'e}moignent de I'{\'e}tablissement d'un couvert v{\'e}g{\'e}tal sur le bassin versant et du lessivage de sols, lors des p{\'e}riodes humides. Les variations d'\&cosyst{\`e}mes et de peuplement sont {\`a} mettre en relation avec I'{\'e}volution du r{\'e}gime hydroclimatique depuis 36 ka, en termes de p{\'e}riodes s{\`e}ches et humides. Petrographic (palynofacies) and geochemical (Rock Eva1 pyrolysis) studies of sedimentary organic matter of a core from a crater lake in Madagascar show a peaty sedimentation before 36 ky and between ca 28 and 15 ky, and between 6 and O ky. Between 36 and 28 ky, the organic sedimentation is characterized by an alternance between phytoplanktonic sedimentation and migrations of vegetation from the basin slope to the lake itself. Contributions of oxidized allochthonous organic matter prove also the presence of vegetation on the surrounding basin and soil leaching. The variation of the ecosystems and their development reveal the hydroclimatic changes during the last 36 kyrs, in terms of arid and humid periods.}},177 keywords = { Lac Tritrivakely, Palynofaci{\`e}s, G{\'e}ochimie organique, Quaternaire sup{\'e}rieur, Pal{\'e}oenvironnements, Madagascar. Lake Tritrivakely, Palynofacies, Organic geochemistry, Late Quaternary, Palaeoenv' o ments, Madagascar.},178 language = { Anglais},179 affiliation = { Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Centre europ{\'e}en de recherche et d'enseignement de g{\'e}osciences de l'environnement - CEREGE , Interactions et dynamique des environnements de surface - IDES},174 title = {{L}a sédimentation organique lacustre en zone tropicale sud au cours des 36 O00 dernières années (Lac {T}ritrivakely, {M}adagascar)}, 175 author = {{A}bdelfettah {S}ifeddine and {F}atima {L}aggoun-{D}éfarge and {E}lisabeth {L}allier-{V}ergès and {J}ean-{R}obert {D}isnar and {D}avid {W}illiamson and {F}rançoise {G}asse and {E}lisabeth {G}ibert}, 176 abstract = {{L'étude pétrographique (palynofaciès) et géochimique (pyrolyse {R}ock {E}val) de la matière organique sédimentaire d'une carotte prélevée dans un lac de cratère de {M}adagascar révèle une sédimentation organique de type tourbeux avant 36 ka, entre ca 28 et 15 ka et entre 6 et O ka, mise en place au cours de périodes d'asséchement. {E}ntre ca 36 et 28 ka, elle se caractérise par une sédimentation lacustre (phytoplancton dominant) et des migrations de végétation du bassin versant vers le lac luimême. {D}es apports de matière organique allochtone témoignent de I'établissement d'un couvert végétal sur le bassin versant et du lessivage de sols, lors des périodes humides. {L}es variations d'\&cosystèmes et de peuplement sont à mettre en relation avec I'évolution du régime hydroclimatique depuis 36 ka, en termes de périodes sèches et humides. {P}etrographic (palynofacies) and geochemical (Rock {E}va1 pyrolysis) studies of sedimentary organic matter of a core from a crater lake in {M}adagascar show a peaty sedimentation before 36 ky and between ca 28 and 15 ky, and between 6 and O ky. {B}etween 36 and 28 ky, the organic sedimentation is characterized by an alternance between phytoplanktonic sedimentation and migrations of vegetation from the basin slope to the lake itself. {C}ontributions of oxidized allochthonous organic matter prove also the presence of vegetation on the surrounding basin and soil leaching. {T}he variation of the ecosystems and their development reveal the hydroclimatic changes during the last 36 kyrs, in terms of arid and humid periods.}}, 177 keywords = {{L}ac {T}ritrivakely, {P}alynofaciès, {G}éochimie organique, {Q}uaternaire supérieur, {P}aléoenvironnements, {M}adagascar. {L}ake {T}ritrivakely, {P}alynofacies, {O}rganic geochemistry, {L}ate {Q}uaternary, {P}alaeoenv' o ments, {M}adagascar.}, 178 language = {{A}nglais}, 179 affiliation = {{P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {C}entre européen de recherche et d'enseignement de géosciences de l'environnement - CEREGE , {I}nteractions et dynamique des environnements de surface - IDES}, 180 180 pages = {385-391}, 181 journal = { Comptes Rendus de l'Acad{\'e}mie des Sciences - Series IIA - Earth and Planetary Science},181 journal = {{C}omptes {R}endus de l'{A}cadémie des {S}ciences - {S}eries IIA - {E}arth and {P}lanetary {S}cience}, 182 182 volume = {321}, 183 183 year = {1995}, … … 189 189 loceanbibid = {01901}, 190 190 timestamp={20121115}, 191 title = {{Lacustrine organic fluxes and palaeoclimatic variations during the last 15 ka: Lac du bouchet (Massif Central, France)}},192 author = { Abdelfettah Sifeddine and Philippe Bertrand and Elisabeth Lallier-Vergès and A.J. Patience},193 abstract = {{To assess the influence of climatic changes on organic lacustrine sedimentation, two cores recovered from the centre of the Lac du Bouchet were studied by petrographical (palynofacies) and geochemical methods. Only core LDB H was used for estimation of the organic fluxes. The variation of these fluxes with climo-stratigraphic periods showed: low organic fluxes during the Lateglacial, an increase at the beginning of the Holocene, a minimum at the end of the Atlantic period resulting from the climatic cooling, and a maximum at the end of the Sub-Boreal related to the installation of the present climatic conditions.}},194 language = { Anglais},195 affiliation = { Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Environnements et Pal{\'e}oenvironnements OC{\'e}aniques - EPOC , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO},191 title = {{Lacustrine organic fluxes and palaeoclimatic variations during the last 15 ka: {L}ac du bouchet (Massif {C}entral, {F}rance)}}, 192 author = {{A}bdelfettah {S}ifeddine and {P}hilippe {B}ertrand and {E}lisabeth {L}allier-{V}ergès and A.J. {P}atience}, 193 abstract = {{To assess the influence of climatic changes on organic lacustrine sedimentation, two cores recovered from the centre of the {L}ac du {B}ouchet were studied by petrographical (palynofacies) and geochemical methods. {O}nly core LDB H was used for estimation of the organic fluxes. {T}he variation of these fluxes with climo-stratigraphic periods showed: low organic fluxes during the {L}ateglacial, an increase at the beginning of the {H}olocene, a minimum at the end of the {A}tlantic period resulting from the climatic cooling, and a maximum at the end of the {S}ub-{B}oreal related to the installation of the present climatic conditions.}}, 194 language = {{A}nglais}, 195 affiliation = {{P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {E}nvironnements et {P}aléoenvironnements OCéaniques - EPOC , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO}, 196 196 pages = {203-211}, 197 journal = { Quaternary Science Reviews},197 journal = {{Q}uaternary {S}cience {R}eviews}, 198 198 volume = {15}, 199 audience = {non sp {\'e}cifi{\'e}e},199 audience = {non spécifiée}, 200 200 doi = {10.1016/0277-3791(95)00078-X}, 201 201 year = {1996}, … … 207 207 loceanbibid = {01900}, 208 208 timestamp={20121115}, 209 title = {{Etude de la sedimentation lacustre d'un site de foret d'altitude des Andes centrales (Bolivie); implications paleoclimatiques}},210 author = { Abdelfettah Sifeddine and Jacques Bertaux and Philippe Mourguiart and Louis Martin and Jean-Robert Disnar and Fatima Laggoun-Défarge and Jaime Argollo},211 abstract = {{A sedimentological study of a 755 cm length core sampled in the middle of a marshy depression surrounded by a cloud forest in the central Andes reveals that this site has recorded important environmental variations during the last 50000 years. For the most part (625 cm) the core is composed of detrital rich sediments deposited during the Upper Pleistocene. The highest amount of detrital influx underlines the Last Glacial Maximum which ranges from ca 29,000 14 C yr B.P. to ca 16,000 14 C yr B.P. (ca 18,500 cal yr B.P.), between two relatively humid phases. The sedimentation of the present Interglacial, starting at ca 12,500 14 C yr B.P. (14,500 cal yr B.P.), is mainly organic, as a consequence of the great development of soils and the forest vegetal cover all over the catchment area. The maximum extension of this vegetal cover ranging from 12,500 to ca 10,500 14 C yr B.P. (14,500 and 12,400 cal yr B.P.) is followed from 10,500 to 8,000 14 C yr B.P. (12,400 and 8,800 cal yr B.P.) by a drier period as revealed by the occurrence of micro-charcoals in the sediment. Between ca 8,000 and 4,000 14 C yr B.P. (8,800 and 4,500 cal yr B.P.), the sharp increase of micro-charcoals content, likely related to palaeofires, underlines an intensification of this dry trend.}},212 language = { Anglais},213 affiliation = { Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO},209 title = {{Etude de la sedimentation lacustre d'un site de foret d'altitude des {A}ndes centrales (Bolivie); implications paleoclimatiques}}, 210 author = {{A}bdelfettah {S}ifeddine and {J}acques {B}ertaux and {P}hilippe {M}ourguiart and {L}ouis {M}artin and {J}ean-{R}obert {D}isnar and {F}atima {L}aggoun-{D}éfarge and {J}aime {A}rgollo}, 211 abstract = {{A sedimentological study of a 755 cm length core sampled in the middle of a marshy depression surrounded by a cloud forest in the central {A}ndes reveals that this site has recorded important environmental variations during the last 50000 years. {F}or the most part (625 cm) the core is composed of detrital rich sediments deposited during the {U}pper {P}leistocene. {T}he highest amount of detrital influx underlines the {L}ast {G}lacial {M}aximum which ranges from ca 29,000 14 C yr B.P. to ca 16,000 14 C yr B.P. (ca 18,500 cal yr B.P.), between two relatively humid phases. {T}he sedimentation of the present {I}nterglacial, starting at ca 12,500 14 C yr B.P. (14,500 cal yr B.P.), is mainly organic, as a consequence of the great development of soils and the forest vegetal cover all over the catchment area. {T}he maximum extension of this vegetal cover ranging from 12,500 to ca 10,500 14 C yr B.P. (14,500 and 12,400 cal yr B.P.) is followed from 10,500 to 8,000 14 C yr B.P. (12,400 and 8,800 cal yr B.P.) by a drier period as revealed by the occurrence of micro-charcoals in the sediment. {B}etween ca 8,000 and 4,000 14 C yr B.P. (8,800 and 4,500 cal yr B.P.), the sharp increase of micro-charcoals content, likely related to palaeofires, underlines an intensification of this dry trend.}}, 212 language = {{A}nglais}, 213 affiliation = {{P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO}, 214 214 pages = {395-402}, 215 journal = { Bulletin de la Soci{\'e}t{\'e} G{\'e}ologique de France},215 journal = {{B}ulletin de la {S}ociété {G}éologique de {F}rance}, 216 216 volume = {169}, 217 217 number = {3}, … … 224 224 loceanbibid = {01899}, 225 225 timestamp={20121115}, 226 title = {{Onocerane testifies to dry climatic events during the Quaternary in the Tropics.}},227 author = { Jérémy Jacob and Jean-Robert Disnar and Mohammed Boussafir and Marie-Pierre Ledru and Ana Luiza Spadano Albuquerque and Abdelfettah Sifeddine and Bruno Turcq},228 abstract = {{An unusual molecular fossil (onocerane I) has been detected for the first time in Quaternary lacustrine sediments (Lagoa do Ca{\c c}{\'o}, NE Brazil). This molecule was initially thought to attest to the former presence of ferns or club mosses. According to possible plant precursors of onocerane-related molecules recorded in the literature and by comparison with palynological results and palaeoclimatic data, we here provide evidence that club mosses and ferns cannot account as sources of onocerane I in this setting. Onocerane I is abundant in the lipid extracts of sediments deposited during the two driest periods recorded in Northern Brazil (Last Glacial Maximum and Younger Dryas). This molecule is therefore suspected to be diagnostic of the development of plants adapted to dry or semi-arid conditions in this region.}},229 language = { Anglais},230 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Universidade de Sao Paulo, Departamento Geologia Sedimentar e Ambiental - IRD/CNPQ , Departamento de Geoquimica - DEPARTAMENTO DE GEOQUIMICA , Departamento de Geoquimica, Universidade Federal Fluminense - IRD/CNPQ , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},226 title = {{Onocerane testifies to dry climatic events during the {Q}uaternary in the {T}ropics.}}, 227 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir and {M}arie-{P}ierre {L}edru and {A}na {L}uiza {S}padano {A}lbuquerque and {A}bdelfettah {S}ifeddine and {B}runo {T}urcq}, 228 abstract = {{An unusual molecular fossil (onocerane I) has been detected for the first time in {Q}uaternary lacustrine sediments (Lagoa do {C}açó, NE {B}razil). {T}his molecule was initially thought to attest to the former presence of ferns or club mosses. {A}ccording to possible plant precursors of onocerane-related molecules recorded in the literature and by comparison with palynological results and palaeoclimatic data, we here provide evidence that club mosses and ferns cannot account as sources of onocerane I in this setting. {O}nocerane I is abundant in the lipid extracts of sediments deposited during the two driest periods recorded in {N}orthern {B}razil (Last {G}lacial {M}aximum and {Y}ounger {D}ryas). {T}his molecule is therefore suspected to be diagnostic of the development of plants adapted to dry or semi-arid conditions in this region.}}, 229 language = {{A}nglais}, 230 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {U}niversidade de {S}ao {P}aulo, {D}epartamento {G}eologia {S}edimentar e {A}mbiental - IRD/CNPQ , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA , {D}epartamento de {G}eoquimica, {U}niversidade {F}ederal {F}luminense - IRD/CNPQ , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 231 231 pages = {289-297}, 232 journal = { Organic Geochemistry},232 journal = {{O}rganic {G}eochemistry}, 233 233 volume = {35}, 234 234 doi = {10.1016/j.orggeochem.2003.11.005}, … … 241 241 loceanbibid = {01898}, 242 242 timestamp={20121115}, 243 title = {{Major environmental changes recorded by lacustrine sedimentary organic matter since the Last Glacial Maximum near the Equator (Lagoa do Ca{\c c}{\'o}, NE Brazil).}},244 author = { Jérémy Jacob and Jean-Robert Disnar and Mohammed Boussafir and Abdelfettah Sifeddine and Bruno Turcq and Ana Luiza Spadano Albuquerque},245 abstract = {{Sediment samples collected along a 6-m core, drilled in the deepest part of the Lagoa do Ca{\c c}{\'o} (NE Brazil), have been investigated in order to determine source(s) and degradation conditions of the organic matter (OM) with special emphasis on paleoenvironmental implications. Bulk organic geochemistry (Rock-Eval pyrolysis, C/N determination, $\delta$13C and $\delta$15N measurement) and petrography combined with sedimentological evidence and radiocarbon dates allowed to identify four major intervals documenting major environmental changes that occurred during the last 20,000 years. The first interval, dating back to the end of the Last Glacial Maximum (LGM), contains well-preserved OM derived from higher plants. This material was most probably produced in an ephemeral palustrine system and rapidly buried by sands. This level is thought to have been deposited under relatively arid climate conditions associated with strong but episodic rainfalls. Between 19,240 and 17,250 Cal years BP, the climate appears to have been more humid and seasonality more pronounced as suggested by the presence of a permanent lake. After a drastic environmental change dating back to 17,250 Cal years BP, the sediment became truly lacustrine with restricted mineral input and highly degraded higher plant-derived organic matter. After that, a stepwise improvement in the preservation of OM occurred, as revealed by several pronounced shifts in the Rock-Eval TpS2 signal. These changes could document abrupt climatically driven changes during the Late Glacial. Finally, around 5610 Cal years BP, environmental conditions, approaching those prevailing today were established. Minor climatic changes during the Holocene were probably buffered by a high water table which might explain the lack of paleoenvironmental fluctuations.}},246 keywords = { Brazil; Lacustrine organic matter; Paleoenvironments; Paleoclimate; Rock-Eval; Organic petrography},247 language = { Anglais},248 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Departamento de Geoquimica Universidade Federal Fluminense, Morro do Valonguinho - DEPARTAMENTO DE GEOQUIMICA , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},243 title = {{Major environmental changes recorded by lacustrine sedimentary organic matter since the {L}ast {G}lacial {M}aximum near the {E}quator (Lagoa do {C}açó, NE {B}razil).}}, 244 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir and {A}bdelfettah {S}ifeddine and {B}runo {T}urcq and {A}na {L}uiza {S}padano {A}lbuquerque}, 245 abstract = {{Sediment samples collected along a 6-m core, drilled in the deepest part of the {L}agoa do {C}açó (NE {B}razil), have been investigated in order to determine source(s) and degradation conditions of the organic matter (OM) with special emphasis on paleoenvironmental implications. {B}ulk organic geochemistry (Rock-{E}val pyrolysis, C/N determination, $\delta$13C and $\delta$15N measurement) and petrography combined with sedimentological evidence and radiocarbon dates allowed to identify four major intervals documenting major environmental changes that occurred during the last 20,000 years. {T}he first interval, dating back to the end of the {L}ast {G}lacial {M}aximum (LGM), contains well-preserved OM derived from higher plants. {T}his material was most probably produced in an ephemeral palustrine system and rapidly buried by sands. {T}his level is thought to have been deposited under relatively arid climate conditions associated with strong but episodic rainfalls. {B}etween 19,240 and 17,250 {C}al years BP, the climate appears to have been more humid and seasonality more pronounced as suggested by the presence of a permanent lake. {A}fter a drastic environmental change dating back to 17,250 {C}al years BP, the sediment became truly lacustrine with restricted mineral input and highly degraded higher plant-derived organic matter. {A}fter that, a stepwise improvement in the preservation of OM occurred, as revealed by several pronounced shifts in the {R}ock-{E}val {T}pS2 signal. {T}hese changes could document abrupt climatically driven changes during the {L}ate {G}lacial. {F}inally, around 5610 {C}al years BP, environmental conditions, approaching those prevailing today were established. {M}inor climatic changes during the {H}olocene were probably buffered by a high water table which might explain the lack of paleoenvironmental fluctuations.}}, 246 keywords = {{B}razil; {L}acustrine organic matter; {P}aleoenvironments; {P}aleoclimate; {R}ock-{E}val; {O}rganic petrography}, 247 language = {{A}nglais}, 248 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {D}epartamento de {G}eoquimica {U}niversidade {F}ederal {F}luminense, {M}orro do {V}alonguinho - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 249 249 pages = {183-197}, 250 journal = { Palaeogeography, Palaeclimatology, Palaeoecology},250 journal = {{P}alaeogeography, {P}alaeclimatology, {P}alaeoecology}, 251 251 volume = {205}, 252 252 doi = {10.1016/j.palaeo.2003.12.005}, … … 259 259 loceanbibid = {01897}, 260 260 timestamp={20121115}, 261 title = {{Quantitative reconstructions of hydrological conditions in Africa 6000 years ago: model-data comparison}},262 author = { Odile Peyron and Dominique Jolly and Pascale Braconnot and Raymonde Bonnefille and Joel Guiot and Denis Wirrmann and Françoise Chalie},263 language = { Anglais},264 affiliation = { Laboratoire Chrono-environnement , Institut des Sciences de l'Evolution - Montpellier - ISEM , Laboratoire des sciences du climat et de l'environnement - LSCE , Centre europ{\'e}en de recherche et d'enseignement de g{\'e}osciences de l'environnement - CEREGE , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},261 title = {{Quantitative reconstructions of hydrological conditions in {A}frica 6000 years ago: model-data comparison}}, 262 author = {{O}dile {P}eyron and {D}ominique {J}olly and {P}ascale {B}raconnot and {R}aymonde {B}onnefille and {J}oel {G}uiot and {D}enis {W}irrmann and {F}rançoise {C}halie}, 263 language = {{A}nglais}, 264 affiliation = {{L}aboratoire {C}hrono-environnement , {I}nstitut des {S}ciences de l'{E}volution - {M}ontpellier - ISEM , {L}aboratoire des sciences du climat et de l'environnement - LSCE , {C}entre européen de recherche et d'enseignement de géosciences de l'environnement - CEREGE , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 265 265 pages = {D24110}, 266 journal = { Journal of Geophysical Research},266 journal = {{J}ournal of {G}eophysical {R}esearch}, 267 267 volume = {111}, 268 268 audience = {internationale}, 269 collaboration = { Projet europeen PMIP1},269 collaboration = {{P}rojet europeen PMIP1}, 270 270 doi = {10.1029/2006JD007396}, 271 271 year = {2006}, … … 278 278 url = {http://hal.archives-ouvertes.fr/hal-00414383}, 279 279 title = {{A rapid calibration procedures for mollusc and coral proxies based on recognition of the environment recording unit}}, 280 author = {J.P. Cuif and Y. Dauphin and N. Guzman and C. E. Lazareth and Luc Ortlieb},280 author = {J.P. {C}uif and Y. {D}auphin and N. {G}uzman and C. E. {L}azareth and {L}uc {O}rtlieb}, 281 281 abstract = {{RSTGV-A-148 \& oral presentation}}, 282 language = { Anglais},283 affiliation = { Interactions et dynamique des environnements de surface - IDES},282 language = {{A}nglais}, 283 affiliation = {{I}nteractions et dynamique des environnements de surface - IDES}, 284 284 booktitle = {{RST}}, 285 address = { Strasbourg, France},285 address = {{S}trasbourg, {F}rance}, 286 286 year = {2004}, 287 287 } … … 291 291 loceanbibid = {01895}, 292 292 timestamp={20121115}, 293 title = {{A 4D approach to unravel the impacts of geodynamics, climate and human activities on biogeochemical cycles, hydrological thresholds, and ecosystems: the Rungwe Environmental Science Observatory Network (Tanzania)}},294 author = { D. Williamson and L. Bergonzini and M. Delalande and C. Quantin and D. Majule and A. Delvaux and D. Mbede and P. Barker and L. Bremond and J. Limyu and F. Magongo and E. Mathé and P.Z. Yanda and F. Chalie and J. Guiot and Luc Ortlieb and P. Valimba and A. Vincens and The Reson Team Members (rungwe Environmental Science Observatory Network (reson)) and W. Abdalla},295 language = { Anglais},296 affiliation = { Interactions et dynamique des environnements de surface - IDES},293 title = {{A 4D approach to unravel the impacts of geodynamics, climate and human activities on biogeochemical cycles, hydrological thresholds, and ecosystems: the {R}ungwe {E}nvironmental {S}cience {O}bservatory {N}etwork (Tanzania)}}, 294 author = {{D}. {W}illiamson and L. {B}ergonzini and M. {D}elalande and C. {Q}uantin and D. {M}ajule and A. {D}elvaux and D. {M}bede and P. {B}arker and L. {B}remond and J. {L}imyu and F. {M}agongo and E. {M}athé and P.Z. {Y}anda and F. {C}halie and J. {G}uiot and {L}uc {O}rtlieb and P. {V}alimba and A. {V}incens and {T}he {R}eson {T}eam {M}embers (rungwe {E}nvironmental {S}cience {O}bservatory {N}etwork (reson)) and W. {A}bdalla}, 295 language = {{A}nglais}, 296 affiliation = {{I}nteractions et dynamique des environnements de surface - IDES}, 297 297 booktitle = {{EGU}}, 298 address = {vienne, Autriche},298 address = {vienne, {A}utriche}, 299 299 year = {2008}, 300 300 month = apr, … … 305 305 loceanbibid = {01894}, 306 306 timestamp={20121115}, 307 title = {{The BIOCALC Project : an European collaborative program aiming at precising the environment recording mechanism in calcareous biominerals through an analysis of the organic/mineral interactions during the biomineralization process}},308 author = { J.P. Cuif and J. Bijma and M. Cusack and Y. Dauphin and J. Doucet and A. Juillet-Leclerc and A. Meibom and L. Mercury and Luc Ortlieb},309 language = { Anglais},310 affiliation = { Interactions et dynamique des environnements de surface - IDES , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},311 booktitle = {{Geophysical Research Abstracts}},307 title = {{The BIOCALC {P}roject : an {E}uropean collaborative program aiming at precising the environment recording mechanism in calcareous biominerals through an analysis of the organic/mineral interactions during the biomineralization process}}, 308 author = {{J}.P. {C}uif and J. {B}ijma and M. {C}usack and Y. {D}auphin and J. {D}oucet and A. {J}uillet-{L}eclerc and A. {M}eibom and L. {M}ercury and {L}uc {O}rtlieb}, 309 language = {{A}nglais}, 310 affiliation = {{I}nteractions et dynamique des environnements de surface - IDES , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 311 booktitle = {{Geophysical {R}esearch {A}bstracts}}, 312 312 pages = {1607-7962}, 313 address = { Vienne, Autriche},313 address = {{V}ienne, {A}utriche}, 314 314 volume = {8}, 315 315 number = {09404}, … … 322 322 loceanbibid = {01893}, 323 323 timestamp={20121115}, 324 title = {{BioCalc : une recherche sur les origines de "l'effet vital" au cours de l'enregistrement des param {\`e}tres environnementaux par les biocristaux calcaires (programme ESF EuroCores EuroMinSci)}},325 author = { J.P. Cuif and J. Bijma and M. Cusack and Y. Dauphin and J. Doucet and A. Juillet-Leclerc and A. Meibom and L. Mercury and Luc Ortlieb},326 language = { Fran{\c c}ais},327 affiliation = { Interactions et dynamique des environnements de surface - IDES , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},328 booktitle = {{Biomin {\'e}ralisation 2006}},324 title = {{BioCalc : une recherche sur les origines de "l'effet vital" au cours de l'enregistrement des paramètres environnementaux par les biocristaux calcaires (programme ESF {E}uroCores {E}uroMinSci)}}, 325 author = {{J}.P. {C}uif and J. {B}ijma and M. {C}usack and Y. {D}auphin and J. {D}oucet and A. {J}uillet-{L}eclerc and A. {M}eibom and L. {M}ercury and {L}uc {O}rtlieb}, 326 language = {{F}rançais}, 327 affiliation = {{I}nteractions et dynamique des environnements de surface - IDES , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 328 booktitle = {{Biominéralisation 2006}}, 329 329 pages = {16}, 330 address = { Nancy, France},330 address = {{N}ancy, {F}rance}, 331 331 audience = {internationale}, 332 332 year = {2006}, … … 337 337 loceanbibid = {01892}, 338 338 timestamp={20121115}, 339 title = {{Subdaily growth patterns and organo-mineral nanostructure of the growth layers in the calcitic prisms of the shell of Concholepas concholepas Brugui{\`e}re, 1789 (Gastropoda, Muricidae).}},340 author = { N. Guzman and A.D. Ball and J.P. Cuif and Y. Dauphin and A. Denis and L. Ortlieb},341 language = { Anglais},342 affiliation = { Interactions et dynamique des environnements de surface - IDES},339 title = {{Subdaily growth patterns and organo-mineral nanostructure of the growth layers in the calcitic prisms of the shell of {C}oncholepas concholepas {B}ruguière, 1789 (Gastropoda, {M}uricidae).}}, 340 author = {{N}. {G}uzman and A.D. {B}all and J.P. {C}uif and Y. {D}auphin and A. {D}enis and L. {O}rtlieb}, 341 language = {{A}nglais}, 342 affiliation = {{I}nteractions et dynamique des environnements de surface - IDES}, 343 343 pages = {397-403}, 344 journal = { Microscopy and Microanalysis},344 journal = {{M}icroscopy and {M}icroanalysis}, 345 345 volume = {13}, 346 346 number = {5}, … … 354 354 timestamp={20121115}, 355 355 title = {{Sensitivity study of the DMS atmospheric concentrations and the sulfate aerosol indirect radiative forcing to the DMS source representation}}, 356 author = { O. Boucher and Olivier Aumont and S. Belviso and Emmanuel Cosme and C. Moulin and M. Pham},357 language = { Anglais},358 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire des sciences du climat et de l'environnement - LSCE , Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI},359 booktitle = {{XXVIIth General Assembly of the European Geophysical Society (EGS)}},360 address = { Nice, France},361 note = { Poster},356 author = {{O}. {B}oucher and {O}livier {A}umont and S. {B}elviso and {E}mmanuel {C}osme and C. {M}oulin and M. {P}ham}, 357 language = {{A}nglais}, 358 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire des écoulements géophysiques et industriels - LEGI}, 359 booktitle = {{XXVIIth {G}eneral {A}ssembly of the {E}uropean {G}eophysical {S}ociety (EGS)}}, 360 address = {{N}ice, {F}rance}, 361 note = {{P}oster}, 362 362 year = {2002}, 363 363 } … … 367 367 loceanbibid = {01890}, 368 368 timestamp={20121115}, 369 title = {{DRAKKAR : La circulation oc{\'e}anique de l'Atlantique Nord et des Mers Nordiques : variabilit{\'e}, processus, et interactions avec l'oc{\'e}an global}},370 author = { Th. Penduff and B. Barnier and Anne-Marie Tréguier and Gurvan Madec},371 language = { Fran{\c c}ais},372 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},373 booktitle = {{Journ {\'e}es d'{\'e}valuation du PATOM}},374 address = { Bordeaux, France},369 title = {{DRAKKAR : {L}a circulation océanique de l'{A}tlantique {N}ord et des {M}ers {N}ordiques : variabilité, processus, et interactions avec l'océan global}}, 370 author = {{T}h. {P}enduff and B. {B}arnier and {A}nne-{M}arie {T}réguier and {G}urvan {M}adec}, 371 language = {{F}rançais}, 372 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire de physique des océans - LPO , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 373 booktitle = {{Journées d'évaluation du PATOM}}, 374 address = {{B}ordeaux, {F}rance}, 375 375 year = {2005}, 376 376 month = sep, … … 382 382 timestamp={20121115}, 383 383 title = {{The modelling component of ocean forecasting}}, 384 author = { E. Chassignet and M. Bell and P. Brasseur and G. Evensen and S. Griffies and H. Hulburt and C. Le Provost and Gurvan Madec and J. Mcclean and J. Verron and A. Wallcraft},385 language = { Anglais},386 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},384 author = {{E}. {C}hassignet and M. {B}ell and P. {B}rasseur and G. {E}vensen and S. {G}riffies and H. {H}ulburt and C. {L}e {P}rovost and {G}urvan {M}adec and J. {M}cclean and J. {V}erron and A. {W}allcraft}, 385 language = {{A}nglais}, 386 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire d'études en {G}éophysique et océanographie spatiales - LEGOS , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 387 387 booktitle = {{The proceeding of the the international symposium "En route to GODAE"}}, 388 388 pages = {41}, 389 address = { France},390 audience = {non sp {\'e}cifi{\'e}e},389 address = {{F}rance}, 390 audience = {non spécifiée}, 391 391 year = {2002}, 392 392 } … … 396 396 loceanbibid = {01888}, 397 397 timestamp={20121115}, 398 title = {{Temporal and Spatial Structure of the Eddy Flow in the Atlantic Ocean Between 1980 and 2000: Validation of the 1/6° CLIPPER Model Simulation Versus the WOCE Current Meter Database}},399 author = { B. Barnier and Th. Penduff and C. Le Delliou and Jean-Marc Molines and Anne-Marie Tréguier and Gurvan Madec and C. Le Provost},400 language = { Anglais},401 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS},402 booktitle = {{The proceeding of the European Geophysical Society}},403 publisher = {ISSN : 1029-7006. Edited by EGS},398 title = {{Temporal and {S}patial {S}tructure of the {E}ddy {F}low in the {A}tlantic {O}cean {B}etween 1980 and 2000: {V}alidation of the 1/6° CLIPPER {M}odel {S}imulation {V}ersus the WOCE {C}urrent {M}eter {D}atabase}}, 399 author = {{B}. {B}arnier and {T}h. {P}enduff and C. {L}e {D}elliou and {J}ean-{M}arc {M}olines and {A}nne-{M}arie {T}réguier and {G}urvan {M}adec and C. {L}e {P}rovost}, 400 language = {{A}nglais}, 401 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire de physique des océans - LPO , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire d'études en {G}éophysique et océanographie spatiales - LEGOS}, 402 booktitle = {{The proceeding of the {E}uropean {G}eophysical {S}ociety}}, 403 publisher = {ISSN : 1029-7006. {E}dited by EGS}, 404 404 pages = {1 page}, 405 address = { Nice, France},406 audience = {non sp {\'e}cifi{\'e}e},405 address = {{N}ice, {F}rance}, 406 audience = {non spécifiée}, 407 407 year = {2003}, 408 408 } … … 412 412 loceanbibid = {01887}, 413 413 timestamp={20121115}, 414 title = {{DRAKKAR: Realistic ice-ocean models to support space oceanography}},415 author = { Th. Penduff and B. Barnier and Anne-Marie Tréguier and C. B{\"o}ning and Gurvan Madec and S. Gulev},416 language = { Anglais},417 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},418 booktitle = {{The proceeding of the Ocean Surface Topography Science Team Meeting}},414 title = {{DRAKKAR: {R}ealistic ice-ocean models to support space oceanography}}, 415 author = {{T}h. {P}enduff and B. {B}arnier and {A}nne-{M}arie {T}réguier and C. {B}öning and {G}urvan {M}adec and S. {G}ulev}, 416 language = {{A}nglais}, 417 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire de physique des océans - LPO , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 418 booktitle = {{The proceeding of the {O}cean {S}urface {T}opography {S}cience {T}eam {M}eeting}}, 419 419 pages = {1 page}, 420 address = {St Petersburg - Florida, {\'E}tats-Unis}, 421 audience = {non sp{\'e}cifi{\'e}e}, 420 address = {{S}t {P}etersburg - {F}lorida, {É}tats-{U}nis}, 422 421 year = {2004}, 423 422 } 424 425 423 @inproceedings{TreguierBarnierEtAl:RCCISC:2006, 426 424 hal_id = {hal-00252101}, 427 425 loceanbibid = {01886}, 428 426 timestamp={20121115}, 429 title = {{Internal and forced variability along a section between Greenland and Portugal in the Clipper Atlantic model}},430 author = { Anne-Marie Tréguier and B. Barnier and C. Gourcuff and P. Lherminier and Gurvan Madec and H. Mercier and Th. Penduff and L. Czeschel and C. Boening},431 language = { Anglais},432 affiliation = { Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},433 booktitle = {{The proceeding of the Rapid Climate Change International Science Conference}},427 title = {{Internal and forced variability along a section between {G}reenland and {P}ortugal in the {C}lipper {A}tlantic model}}, 428 author = {{A}nne-{M}arie {T}réguier and B. {B}arnier and C. {G}ourcuff and P. {L}herminier and {G}urvan {M}adec and H. {M}ercier and {T}h. {P}enduff and L. {C}zeschel and C. {B}oening}, 429 language = {{A}nglais}, 430 affiliation = {{L}aboratoire de physique des océans - LPO , {L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 431 booktitle = {{The proceeding of the {R}apid {C}limate {C}hange {I}nternational {S}cience {C}onference}}, 434 432 pages = {1 page}, 435 address = { Birmingham, Royaume-Uni},436 audience = {non sp {\'e}cifi{\'e}e},433 address = {{B}irmingham, {R}oyaume-{U}ni}, 434 audience = {non spécifiée}, 437 435 year = {2006}, 438 436 } … … 444 442 title = {{Influence of numerical schemes on current-topography interactions in 1/4° global ocean simulations}}, 445 443 author = {{T}hierry {P}enduff and {J}ulien {{L}e {S}ommer} and {B}ernard {B}arnier and {A}nne-{M}arie {T}réguier and {J}ean-{M}arc {M}olines and {G}urvan {M}adec}, 446 language = { Anglais},447 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},448 booktitle = {{Proc. Workshop on Numerical Methods in Ocean Models}},449 pages = {pas pr {\'e}cise},450 address = {bergen, Norv{\`e}ge},444 language = {{A}nglais}, 445 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 446 booktitle = {{Proc. {W}orkshop on {N}umerical {M}ethods in {O}cean {M}odels}}, 447 pages = {pas précise}, 448 address = {bergen, {N}orvège}, 451 449 audience = {internationale}, 452 450 year = {2007}, … … 457 455 loceanbibid = {01884}, 458 456 timestamp={20121115}, 459 title = {{Interannual-to-decadal variability of North Atlantic air-sea CO2 fluxes}},460 author = { S. Raynaud and Olivier Aumont and K. B. Rodgers and P. Yiou and J. C. Orr},461 abstract = {{The magnitude of the interannual variability of North Atlantic air-sea CO2 fluxes remains uncertain. Fluxes inferred from atmospheric inversions have large variability, whereas those simulated by ocean models have small variability. Part of the difference is that unlike typical atmospheric inversions, ocean models come with spatial resolution at the sub-basin scale. Here we explore sub-basin-scale spatiotemporal variability in the North Atlantic in one ocean model in order to better understand why the the North Atlantic basin may well contribute very little to the global variability of air-sea CO2 flux. We made two simulations with a biogeochemical model coupled to a global ocean general circulation model (OGCM), which itself was forced by 55-year NCEP reanalysis fields. In the first simulation, atmospheric CO2 was maintained at the preindustrial level (278 ppmv); in the second simulation, atmospheric CO2 followed the observed increase. Simulated air-sea CO2 fluxes and associated variables were analysed with a statistical tool known as multichannel singular spectrum analysis (MSSA). We found that the subtropical gyre is not the largest contributor to the overall, basin-wide variability, in contrast to previous suggestions. The subpolar gyre and the inter-gyre region (the transition area between subpolar and subtropical gyres) also contribute with multipolar anomalies at multiple frequencies: these tend to cancel one another in terms of the basin-wide air-sea CO2 flux. We found a strong correlation between the air-sea CO2 fluxes and the North Atlantic Oscillation (NAO), but only if one takes into account time lags as does MSSA (maximum r=0.64 for lags between 1 and 3 years). The contribution of anthropogenic CO2 to total variability was negligible at interannual time scales, whereas at the decadal (13-year) time scale, it increased variability by 30\%.}},462 language = { Anglais},463 affiliation = { Laboratoire des sciences du climat et de l'environnement - LSCE , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},457 title = {{Interannual-to-decadal variability of {N}orth {A}tlantic air-sea CO2 fluxes}}, 458 author = {{S}. {R}aynaud and {O}livier {A}umont and K. B. {R}odgers and P. {Y}iou and J. C. {O}rr}, 459 abstract = {{The magnitude of the interannual variability of {N}orth {A}tlantic air-sea CO2 fluxes remains uncertain. {F}luxes inferred from atmospheric inversions have large variability, whereas those simulated by ocean models have small variability. {P}art of the difference is that unlike typical atmospheric inversions, ocean models come with spatial resolution at the sub-basin scale. {H}ere we explore sub-basin-scale spatiotemporal variability in the {N}orth {A}tlantic in one ocean model in order to better understand why the the {N}orth {A}tlantic basin may well contribute very little to the global variability of air-sea CO2 flux. {W}e made two simulations with a biogeochemical model coupled to a global ocean general circulation model (OGCM), which itself was forced by 55-year NCEP reanalysis fields. {I}n the first simulation, atmospheric CO2 was maintained at the preindustrial level (278 ppmv); in the second simulation, atmospheric CO2 followed the observed increase. {S}imulated air-sea CO2 fluxes and associated variables were analysed with a statistical tool known as multichannel singular spectrum analysis (MSSA). {W}e found that the subtropical gyre is not the largest contributor to the overall, basin-wide variability, in contrast to previous suggestions. {T}he subpolar gyre and the inter-gyre region (the transition area between subpolar and subtropical gyres) also contribute with multipolar anomalies at multiple frequencies: these tend to cancel one another in terms of the basin-wide air-sea CO2 flux. {W}e found a strong correlation between the air-sea CO2 fluxes and the {N}orth {A}tlantic {O}scillation (NAO), but only if one takes into account time lags as does MSSA (maximum r=0.64 for lags between 1 and 3 years). {T}he contribution of anthropogenic CO2 to total variability was negligible at interannual time scales, whereas at the decadal (13-year) time scale, it increased variability by 30\%.}}, 460 language = {{A}nglais}, 461 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 464 462 pages = {437-472}, 465 journal = { Ocean Science Discussions},463 journal = {{O}cean {S}cience {D}iscussions}, 466 464 volume = {2}, 467 465 number = {4}, … … 476 474 loceanbibid = {01883}, 477 475 timestamp={20121115}, 478 title = {{In situ building of dunes since the Sub Boreal (3600 BP): evidence of chronological continuity on the northern coast of Brittany. An example in Anse du Verger (Ille-et-Vilaine)}},479 author = { Hervé Regnauld and Jean-François Saliège and Jérôme Fournier and Jean-Yves Cocaign},480 abstract = {{A series of storms, from 1990 to 1995, has revealed new cross-sections on the Northern Coast of Brittany, more specifically close to St-Malo, in the Anse du Verger (Verger cove). They have also allowed the effects of storms surges on coastal features to be followed. An anthropogenic shell layer, discovered in a dune and dated from 3640 (conventional BP) is covered by a storms surge deposit, dated from 2460, conventional BP. A comparison between present and sub-boreal surges is attempted. Then a chronology for dune building is proposed, in relation with sea level rise and surges. The possibility of an accumulation feature rising itself instead of retreating before an increasing sea level is proposed.}},481 keywords = { Storm surge ; Shell deposits ; Holocene dunes ; Sea level},482 language = { Fran{\c c}ais},483 affiliation = { Littoral, Environnement, T{\'e}l{\'e}d{\'e}tection, G{\'e}omatique - LETG - Costel , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Civilisations atlantiques \& Arch{\'e}osciences - C2A},476 title = {{In situ building of dunes since the {S}ub {B}oreal (3600 BP): evidence of chronological continuity on the northern coast of {B}rittany. {A}n example in {A}nse du {V}erger (Ille-et-{V}ilaine)}}, 477 author = {{H}ervé {R}egnauld and {J}ean-{F}rançois {S}aliège and {J}érôme {F}ournier and {J}ean-{Y}ves {C}ocaign}, 478 abstract = {{A series of storms, from 1990 to 1995, has revealed new cross-sections on the {N}orthern {C}oast of {B}rittany, more specifically close to {S}t-{M}alo, in the {A}nse du {V}erger (Verger cove). {T}hey have also allowed the effects of storms surges on coastal features to be followed. {A}n anthropogenic shell layer, discovered in a dune and dated from 3640 (conventional BP) is covered by a storms surge deposit, dated from 2460, conventional BP. A comparison between present and sub-boreal surges is attempted. {T}hen a chronology for dune building is proposed, in relation with sea level rise and surges. {T}he possibility of an accumulation feature rising itself instead of retreating before an increasing sea level is proposed.}}, 479 keywords = {{S}torm surge ; {S}hell deposits ; {H}olocene dunes ; {S}ea level}, 480 language = {{F}rançais}, 481 affiliation = {{L}ittoral, {E}nvironnement, {T}élédétection, {G}éomatique - LETG - {C}ostel , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {C}ivilisations atlantiques \& {A}rchéosciences - C2A}, 484 482 pages = {303-310}, 485 journal = { Comptes Rendus de l'Academie des Sciences. Serie II, Sciences de la Terre et des planetes},483 journal = {{C}omptes {R}endus de l'{A}cademie des {S}ciences. {S}erie II, {S}ciences de la {T}erre et des planetes}, 486 484 volume = {321}, 487 485 year = {1995}, … … 492 490 loceanbibid = {01882}, 493 491 timestamp={20121115}, 494 title = {{A four-dimensional mesoscale map of the spring bloom in the northeast Atlantic (POMME experiment): Results of a prognostic model}},495 author = { Marina Lévy and M. Gavart and Laurent Mémery and Guy Caniaux and A. Paci},496 language = { Anglais},497 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Service Hydrographique et Oc{\'e}anographique de la Marine - SHOM , Laboratoire des Sciences de l'Environnement Marin - LEMAR , Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME},492 title = {{A four-dimensional mesoscale map of the spring bloom in the northeast {A}tlantic (POMME experiment): {R}esults of a prognostic model}}, 493 author = {{M}arina {L}évy and M. {G}avart and {L}aurent {M}émery and {G}uy {C}aniaux and A. {P}aci}, 494 language = {{A}nglais}, 495 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {S}ervice {H}ydrographique et {O}céanographique de la {M}arine - SHOM , {L}aboratoire des {S}ciences de l'{E}nvironnement {M}arin - LEMAR , {G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME}, 498 496 pages = {C07S21}, 499 journal = { Journal of Geophysical Research},497 journal = {{J}ournal of {G}eophysical {R}esearch}, 500 498 volume = {110}, 501 audience = {non sp {\'e}cifi{\'e}e},499 audience = {non spécifiée}, 502 500 doi = {10.1029/2004JC002588}, 503 501 year = {2005}, … … 508 506 loceanbibid = {01881}, 509 507 timestamp={20121115}, 510 title = {{On the relationship between satellite-retrieved surface temperature fronts and chlorophyll a in the western South Atlantic}},511 author = { Martin Saraceno and Christine Provost and Alberto R. Piola},512 language = { Anglais},513 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Departamento de Oceanograf{\'\i}a , Departamento de Ciencias de la Atm{\'o}sfera y los Oc{\'e}anos, Facultad de Ciencias Exactas y Naturales},508 title = {{On the relationship between satellite-retrieved surface temperature fronts and chlorophyll a in the western {S}outh {A}tlantic}}, 509 author = {{M}artin {S}araceno and {C}hristine {P}rovost and {A}lberto R. {P}iola}, 510 language = {{A}nglais}, 511 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {D}epartamento de {O}ceanografìa , {D}epartamento de {C}iencias de la {A}tmósfera y los {O}céanos, {F}acultad de {C}iencias {E}xactas y {N}aturales}, 514 512 pages = {C11016}, 515 journal = { Journal of Geophysical Research},513 journal = {{J}ournal of {G}eophysical {R}esearch}, 516 514 volume = {110}, 517 audience = {non sp {\'e}cifi{\'e}e},515 audience = {non spécifiée}, 518 516 doi = {10.1029/2004JC002736}, 519 517 year = {2005}, … … 524 522 loceanbibid = {01880}, 525 523 timestamp={20121115}, 526 title = {{Mesoscale variability of sea surface pCO2: What does it respond to?}},527 author = { A. Mahadevan and Marina Lévy and Laurent Mémery},528 language = { Anglais},529 affiliation = { Department of Earth Sciences , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},524 title = {{Mesoscale variability of sea surface pCO2: {W}hat does it respond to?}}, 525 author = {{A}. {M}ahadevan and {M}arina {L}évy and {L}aurent {M}émery}, 526 language = {{A}nglais}, 527 affiliation = {{D}epartment of {E}arth {S}ciences , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 530 528 pages = {GB1017}, 531 journal = { Global Biogeochemical Cycles},529 journal = {{G}lobal {B}iogeochemical {C}ycles}, 532 530 volume = {18}, 533 audience = {non sp {\'e}cifi{\'e}e},531 audience = {non spécifiée}, 534 532 doi = {10.1029/2003GB002102}, 535 533 year = {2004}, … … 540 538 loceanbibid = {01879}, 541 539 timestamp={20121115}, 542 title = {{Distributions of oxygen and carbon stable isotopes and CFC-12 in the water masses of the Southern Ocean at 30°E from South Africa to Antarctica: results of the CIVA1 cruise}},543 author = { Anne-Sophie Archambeau and Catherine Pierre and Alain Poisson and Bernard Schauer},544 abstract = {{This study presents oceanic distributions of stable isotopes ($\delta$18O of water and $\delta$13C of $\Sigma$CO2) and CFC-12 from samples collected during the CIVA1 cruise (February/March 1993), across the Southern Ocean, along a meridian section at 30°E, from South Africa (44°S) to Antarctica (70°S). The isotopic measurements show important variations between the subantarctic surface waters with low $\delta$18O--high $\delta$13C values and the antarctic surface waters with very low $\delta$18O--low $\delta$13C values. The surface distributions of $\delta$13C values follow the major frontal oceanic structures; the vertical distribution shows the progressive upwelling from the subantarctic zone to the antarctic divergence of 13C-depleted CO2 derived from remineralization of organic matter. Along the Antarctic continental shelf, between 2500 and 4000 m, a core of water with $\delta$18O values close to --0.1 is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. This water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the Weddell gyre or from bottom waters coming from the East and formed near Prydz Bay.}},545 keywords = { Stable isotopes; 18O; 13C; CFC-12; Austral Ocean},546 language = { Anglais},547 affiliation = { Laboratoire de Physique et Chimie Marines - LPCM , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},540 title = {{Distributions of oxygen and carbon stable isotopes and CFC-12 in the water masses of the {S}outhern {O}cean at 30°E from {S}outh {A}frica to {A}ntarctica: results of the CIVA1 cruise}}, 541 author = {{A}nne-{S}ophie {A}rchambeau and {C}atherine {P}ierre and {A}lain {P}oisson and {B}ernard {S}chauer}, 542 abstract = {{This study presents oceanic distributions of stable isotopes ($\delta$18O of water and $\delta$13C of $\Sigma$CO2) and CFC-12 from samples collected during the CIVA1 cruise (February/March 1993), across the {S}outhern {O}cean, along a meridian section at 30°E, from {S}outh {A}frica (44°S) to {A}ntarctica (70°S). {T}he isotopic measurements show important variations between the subantarctic surface waters with low $\delta$18O--high $\delta$13C values and the antarctic surface waters with very low $\delta$18O--low $\delta$13C values. {T}he surface distributions of $\delta$13C values follow the major frontal oceanic structures; the vertical distribution shows the progressive upwelling from the subantarctic zone to the antarctic divergence of 13C-depleted CO2 derived from remineralization of organic matter. {A}long the {A}ntarctic continental shelf, between 2500 and 4000 m, a core of water with $\delta$18O values close to --0.1 is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. {T}his water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the {W}eddell gyre or from bottom waters coming from the {E}ast and formed near {P}rydz {B}ay.}}, 543 keywords = {{S}table isotopes; 18O; 13C; CFC-12; {A}ustral {O}cean}, 544 language = {{A}nglais}, 545 affiliation = {{L}aboratoire de {P}hysique et {C}himie {M}arines - LPCM , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 548 546 pages = {25-38}, 549 journal = { Journal of Marine Systems},547 journal = {{J}ournal of {M}arine {S}ystems}, 550 548 volume = {17}, 551 549 number = {1-4}, … … 561 559 loceanbibid = {01878}, 562 560 timestamp={20121014}, 563 title = {{L' {\'e}pid{\'e}mie de m{\'e}ningite au Mali et la circulation atmosph{\'e}rique en Afrique de l'Ouest}},564 author = { Benjamin Sultan and K. Labadi and G. Beltrando and Serge Janicot},565 language = { Fran{\c c}ais},566 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},561 title = {{L'épidémie de méningite au {M}ali et la circulation atmosphérique en {A}frique de l'{O}uest}}, 562 author = {{B}enjamin {S}ultan and K. {L}abadi and G. {B}eltrando and {S}erge {J}anicot}, 563 language = {{F}rançais}, 564 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 567 565 pages = {23-34}, 568 journal = { Environnement, Risques et Sant{\'e}},566 journal = {{E}nvironnement, {R}isques et {S}anté}, 569 567 volume = {3}, 570 568 number = {1}, 571 audience = {non sp {\'e}cifi{\'e}e},569 audience = {non spécifiée}, 572 570 year = {2004}, 573 571 } … … 578 576 timestamp={20121014}, 579 577 title = {{Extended deep equatorial layering as a possible imprint of inertial instability.}}, 580 author = { M. D'Orgeville and B. L. Hua and R. Schopp and L. Bunge},581 abstract = {{The deep equatorial track of the world ocean is subject to intense zonal flow fields that still remain to be better understood. Inertial instability has been invoked to explain some of its features. Here we present possible in situ imprints of such a mechanism in the equatorial Atlantic Ocean below the thermocline. We analyse the observed pattern of homogeneous density layers of 50--100 m vertical scale, which are characterized by a large meridional coherency up to 2° of latitude, a concentration in the vicinity of the equator and foremost a vertical localization within regions of well-mixed angular momentum (westward jets). These distinctive properties suggest inertial instability to be a plausible mechanism for this extended layering. Numerical simulations forced by a time-oscillating shear reproduce the observed density layering characteristics. The prescription of deep jets in the background flow controls the vertical localization of the layering inside westward jets.}},582 language = { Anglais},583 affiliation = { Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},578 author = {{M}. D'{O}rgeville and B. L. {H}ua and R. {S}chopp and L. {B}unge}, 579 abstract = {{The deep equatorial track of the world ocean is subject to intense zonal flow fields that still remain to be better understood. {I}nertial instability has been invoked to explain some of its features. {H}ere we present possible in situ imprints of such a mechanism in the equatorial {A}tlantic {O}cean below the thermocline. {W}e analyse the observed pattern of homogeneous density layers of 50--100 m vertical scale, which are characterized by a large meridional coherency up to 2° of latitude, a concentration in the vicinity of the equator and foremost a vertical localization within regions of well-mixed angular momentum (westward jets). {T}hese distinctive properties suggest inertial instability to be a plausible mechanism for this extended layering. {N}umerical simulations forced by a time-oscillating shear reproduce the observed density layering characteristics. {T}he prescription of deep jets in the background flow controls the vertical localization of the layering inside westward jets.}}, 580 language = {{A}nglais}, 581 affiliation = {{L}aboratoire de physique des océans - LPO , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 584 582 pages = {L22303}, 585 journal = { Geophysical Research Letters},583 journal = {{G}eophysical {R}esearch {L}etters}, 586 584 volume = {31}, 587 585 audience = {internationale}, … … 594 592 loceanbibid = {01876}, 595 593 timestamp={20121014}, 596 title = {{Organic-rich sediments in ventilated deep-sea environments: Relationship to climate, sea level, and trophic changes}},597 author = { Philippe Bertrand and T. F. Pedersen and R. Schneider and G. Shimmield and Elisabeth Lallier-Vergès and Jean-Robert Disnar and D. Massias and J. Villanueva and Nicolas Tribovillard and Alain-Yves Huc and X. Giraud and Catherine Pierre and M.T. Vénec-Peyré},598 abstract = {{Sediments on the Namibian Margin in the SE Atlantic between water depths of $\sim$1000 and $\sim$3600 m are highly enriched in hydrocarbon-prone organic matter. Such sedimentation has occurred for more than 2 million years and is geographically distributed over hundreds of kilometers along the margin, so that the sediments of this region contain a huge concentrated stock of organic carbon. It is shown here that most of the variability in organic content is due to relative dilution by buried carbonates. This reflects both export productivity and diagenetic dissolution, not differences in either water column or bottom water anoxia and related enhanced preservation of organic matter. These observations offer a new mechanism for the formation of potential source rocks in a well-ventilated open ocean, in this case the South Atlantic. The organic richness is discussed in terms of a suite of probable controls including local wind-driven productivity (upwelling), trophic conditions, transfer efficiency, diagenetic processes, and climate-related sea level and deep circulation. The probability of past occurrences of such organic-rich facies in equivalent oceanographic settings at the edge of large oceanic basins should be carefully considered in deep offshore exploration.}},599 language = { Anglais},600 affiliation = { Environnements et Pal{\'e}oenvironnements OC{\'e}aniques - EPOC , Oceanography, Earth and Ocean Sciences , Fachbereicht Geowissenschaften, Universit{\"a}t Bremen , Dunstaffnage Marine Laboratory , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Processus et bilan des domaines s{\'e}dimentaires - PBDS , IFP Energies Nouvelles - IFPEN , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire de min{\'e}ralogie du Mus{\'e}um National d'Histoire Naturelle - LMMNHN},594 title = {{Organic-rich sediments in ventilated deep-sea environments: {R}elationship to climate, sea level, and trophic changes}}, 595 author = {{P}hilippe {B}ertrand and T. F. {P}edersen and R. {S}chneider and G. {S}himmield and {E}lisabeth {L}allier-{V}ergès and {J}ean-{R}obert {D}isnar and D. {M}assias and J. {V}illanueva and {N}icolas {T}ribovillard and {A}lain-{Y}ves {H}uc and X. {G}iraud and {C}atherine {P}ierre and M.T. {V}énec-{P}eyré}, 596 abstract = {{Sediments on the {N}amibian {M}argin in the SE {A}tlantic between water depths of $\sim$1000 and $\sim$3600 m are highly enriched in hydrocarbon-prone organic matter. {S}uch sedimentation has occurred for more than 2 million years and is geographically distributed over hundreds of kilometers along the margin, so that the sediments of this region contain a huge concentrated stock of organic carbon. {I}t is shown here that most of the variability in organic content is due to relative dilution by buried carbonates. {T}his reflects both export productivity and diagenetic dissolution, not differences in either water column or bottom water anoxia and related enhanced preservation of organic matter. {T}hese observations offer a new mechanism for the formation of potential source rocks in a well-ventilated open ocean, in this case the {S}outh {A}tlantic. {T}he organic richness is discussed in terms of a suite of probable controls including local wind-driven productivity (upwelling), trophic conditions, transfer efficiency, diagenetic processes, and climate-related sea level and deep circulation. {T}he probability of past occurrences of such organic-rich facies in equivalent oceanographic settings at the edge of large oceanic basins should be carefully considered in deep offshore exploration.}}, 597 language = {{A}nglais}, 598 affiliation = {{E}nvironnements et {P}aléoenvironnements OCéaniques - EPOC , {O}ceanography, {E}arth and {O}cean {S}ciences , {F}achbereicht {G}eowissenschaften, {U}niversität {B}remen , {D}unstaffnage {M}arine {L}aboratory , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {P}rocessus et bilan des domaines sédimentaires - PBDS , IFP {E}nergies {N}ouvelles - IFPEN , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire de minéralogie du {M}uséum {N}ational d'{H}istoire {N}aturelle - LMMNHN}, 601 599 pages = {C2, 3045}, 602 journal = { Journal of Geophysical Research},600 journal = {{J}ournal of {G}eophysical {R}esearch}, 603 601 volume = {108}, 604 audience = {non sp {\'e}cifi{\'e}e},602 audience = {non spécifiée}, 605 603 doi = {10.1029/2000JC000327}, 606 604 year = {2003}, … … 612 610 loceanbibid = {01875}, 613 611 timestamp={20121014}, 614 title = {{M {\'e}moire de Titres et Travaux}},615 author = { Nicolas Dégallier},616 abstract = {{A synthesis of all results of researches done by the author on arboviruses cycles and bioecology of their vectors in French Guiana, Central African Republic and Brazil, from 1975 to 1996. Emphasis is put on the ecoepidemiology of yellow fever and dengue viruses. Studies are also reported on the impacts of environmental changes on the transmission of arboviruses in Brazilian Amazonia.An exhaustive list of publications and communications of the author is presented.}},617 keywords = {arbovirus;vecteurs;tiques;moustiques;Culicidae;afrotropical;n {\'e}otropical;{\'e}pid{\'e}miologie;bio{\'e}cologie;environnement},618 language = { Fran{\c c}ais},619 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},620 school = { Universit{\'e} Paris Sud - Paris XI},612 title = {{Mémoire de {T}itres et {T}ravaux}}, 613 author = {{N}icolas {D}égallier}, 614 abstract = {{A synthesis of all results of researches done by the author on arboviruses cycles and bioecology of their vectors in {F}rench {G}uiana, {C}entral {A}frican {R}epublic and {B}razil, from 1975 to 1996. {E}mphasis is put on the ecoepidemiology of yellow fever and dengue viruses. {S}tudies are also reported on the impacts of environmental changes on the transmission of arboviruses in {B}razilian {A}mazonia. An exhaustive list of publications and communications of the author is presented.}}, 615 keywords = {arbovirus;vecteurs;tiques;moustiques;Culicidae;afrotropical;néotropical;épidémiologie;bioécologie;environnement}, 616 language = {{F}rançais}, 617 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 618 school = {{U}niversité {P}aris {S}ud - {P}aris XI}, 621 619 type = {{H}abilitation à {D}iriger des {R}echerches}, 622 620 year = {1996}, … … 631 629 type = {{T}hèse de doctorat}, 632 630 directeur_de_these = {{S}erge {J}anicot}, 633 title = {{Analyse du m{\'e}canisme de la mise en place de la mousson Africaine: dynamique r{\'e}gionale ou for{\c c}age de grande {\'e}chelle?}}, 634 author = {Emmanouil Flaounas}, 635 abstract = {{La saison des pluies en Afrique de l'Ouest est primordiale pour les populations locales. La mise en place de la mousson (MAO) se produit fin juin et correspond {\`a} un affaiblissement global de la convection sur la r{\'e}gion puis une transition brutale des pr{\'e}cipitations de la c{\^o}te de Guin{\'e}e vers le Sahel. C'est le m{\'e}canisme responsable de ce " saut " qui est {\'e}tudi{\'e} ici {\`a} partir d'exp{\'e}riences num{\'e}riques. La capacit{\'e} du mod{\`e}le {\`a} aire limit{\'e}e WRF {\`a} reproduire la circulation de la MAO en 2006 a d'abord {\'e}t{\'e} {\'e}valu{\'e}e. Diff{\'e}rentes param{\'e}trisations de la convection et de la couche limite ont {\'e}t{\'e} test{\'e}es et leur impact sur les simulations analys{\'e}. Des tests de sensibilit{\'e} ont ensuite {\'e}t{\'e} effectu{\'e}s pour {\'e}valuer le r{\^o}le de la d{\'e}pression thermique saharienne et de la SST (m{\'e}canismes propos{\'e}s dans d'autres {\'e}tudes) sur la mise en place de la MAO. Les r{\'e}sultats montrent que la phase de transition d{\'e}pend plus fortement de la dynamique de grande {\'e}chelle que des {\'e}l{\'e}ments r{\'e}gionaux. Plus pr{\'e}cis{\'e}ment, la mise en place de la mousson Indienne lib{\`e}re une onde de Rossby qui se propage vers l'ouest, arrive au dessus de l'Afrique du Nord en favorisant les intrusions de masses d'air sec au dessus de l'Afrique de l'Ouest qui inhibent la convection. En parall{\`e}le, le gradient m{\'e}ridien de pression de surface est renforc{\'e} et la MAO s'intensifie en advectant de l'humidit{\'e} au dessus du Sahel. Une fois l'onde {\'e}vacu{\'e}e, la convection se r{\'e}organise au dessus du Sahel o{\`u} les conditions thermodynamiques sont favorables. L'utilisation de simulations globales avec LMDz a confirm{\'e} le r{\^o}le de la mousson indienne sur toute la p{\'e}riode 1989-2008 avec cependant des ann{\'e}es plus ou moins marqu{\'e}es.}}, 636 keywords = {Mousson Africaine, mise en place}, 637 language = {Fran{\c c}ais}, 638 affiliation = {Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN}, 639 school = {Universit{\'e} Pierre et Marie Curie - Paris VI}, 640 type = {THESE}, 631 title = {{Analyse du mécanisme de la mise en place de la mousson {A}fricaine: dynamique régionale ou forçage de grande échelle?}}, 632 author = {{E}mmanouil {F}laounas}, 633 abstract = {{La saison des pluies en {A}frique de l'{O}uest est primordiale pour les populations locales. {L}a mise en place de la mousson (MAO) se produit fin juin et correspond à un affaiblissement global de la convection sur la région puis une transition brutale des précipitations de la côte de {G}uinée vers le {S}ahel. C'est le mécanisme responsable de ce " saut " qui est étudié ici à partir d'expériences numériques. {L}a capacité du modèle à aire limitée WRF à reproduire la circulation de la MAO en 2006 a d'abord été évaluée. {D}ifférentes paramétrisations de la convection et de la couche limite ont été testées et leur impact sur les simulations analysé. {D}es tests de sensibilité ont ensuite été effectués pour évaluer le rôle de la dépression thermique saharienne et de la SST (mécanismes proposés dans d'autres études) sur la mise en place de la MAO. {L}es résultats montrent que la phase de transition dépend plus fortement de la dynamique de grande échelle que des éléments régionaux. {P}lus précisément, la mise en place de la mousson {I}ndienne libère une onde de {R}ossby qui se propage vers l'ouest, arrive au dessus de l'{A}frique du {N}ord en favorisant les intrusions de masses d'air sec au dessus de l'{A}frique de l'{O}uest qui inhibent la convection. {E}n parallèle, le gradient méridien de pression de surface est renforcé et la MAO s'intensifie en advectant de l'humidité au dessus du {S}ahel. {U}ne fois l'onde évacuée, la convection se réorganise au dessus du {S}ahel où les conditions thermodynamiques sont favorables. L'utilisation de simulations globales avec LMDz a confirmé le rôle de la mousson indienne sur toute la période 1989-2008 avec cependant des années plus ou moins marquées.}}, 634 keywords = {{M}ousson {A}fricaine, mise en place}, 635 language = {{F}rançais}, 636 affiliation = {{L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 637 school = {{U}niversité {P}ierre et {M}arie {C}urie - {P}aris VI}, 641 638 collaboration = {AMMA}, 642 639 year = {2010}, … … 649 646 loceanbibid = {01873}, 650 647 timestamp={20121014}, 651 title = {{La dengue et ses vecteurs au Br{\'e}sil}},652 author = { Nicolas Dégallier and Amélia P.A. Travassos Da Rosa and Pedro F. C. Vasconcelos and Luiz Tadeu Moraes Figueiredo and Jorge F. S. Travassos Da Rosa and Sueli G. Rodrigues and Elisabeth S. Travassos Da Rosa},653 abstract = {{L'histoire de la Dengue au Br{\'e}sil est survol{\'e}e depuis les premi{\`e}res relations d'{\'e}pid{\'e}mies au 19e si{\`e}cle jusqu'aux grands {\'e}pisodes de la derni{\`e}re d{\'e}cennie. Les s{\'e}rotypes DEN 1 and DEN 4 ont {\'e}t{\'e} isol{\'e}s pour la premi{\`e}re fois au Br{\'e}sil en 1982, au cours d'une {\'e}pid{\'e}mie {\`a} Boa Vista, Roraima. En 1986, le virus DEN 1 fut le responsable d'{\'e}pid{\'e}mies {\`a} Rio de Janeiro et dans le Nordeste du Br{\'e}sil. A partir de 1990, le virus DEN 2 {\'e}tait pr{\'e}sent {\'e}galement dans l'int{\'e}rieur du pays et en Amazonie. A Rio de Janeiro (1990-91) et dans l'Etat du Ceara (1994) o{\`u} les deux s{\'e}rotypes DEN 1 et DEN 2 circulaient en m{\^e}me temps, plusieurs cas de DHS/DSS ont {\'e}t{\'e} signal{\'e}s. Environ 500000 cas de Dengue ont {\'e}t{\'e} notifi{\'e}s de 1982 {\`a} 1994. Aedes aegypti est le seul vecteur urbain {\`a} partir duquel 4 souches de DEN 4, 7 souches de DEN 1 et 16 souches de DEN 2 ont {\'e}t{\'e} isol{\'e}es. La transmission transovarienne ne semble pas avoir lieu chez cette esp{\`e}ce au Br{\'e}sil.}},654 keywords = { Dengue 1; Dengue 2; Dengue 4; Aedes aegypti; Aedes albopictus; Br{\'e}sil; histoire; epid{\'e}miologie},655 language = { Fran{\c c}ais},656 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratorio de Arbovirus , Unit{\'e} de recherches en virologie , Institut Evandro Chagas-FNS},648 title = {{La dengue et ses vecteurs au {B}résil}}, 649 author = {{N}icolas {D}égallier and {A}mélia P.A. {T}ravassos {D}a {R}osa and {P}edro F. C. {V}asconcelos and {L}uiz {T}adeu {M}oraes {F}igueiredo and {J}orge F. S. {T}ravassos {D}a {R}osa and {S}ueli G. {R}odrigues and {E}lisabeth S. {T}ravassos {D}a {R}osa}, 650 abstract = {{L'histoire de la {D}engue au {B}résil est survolée depuis les premières relations d'épidémies au 19e siècle jusqu'aux grands épisodes de la dernière décennie. {L}es sérotypes DEN 1 and DEN 4 ont été isolés pour la première fois au {B}résil en 1982, au cours d'une épidémie à {B}oa {V}ista, {R}oraima. {E}n 1986, le virus DEN 1 fut le responsable d'épidémies à {R}io de {J}aneiro et dans le {N}ordeste du {B}résil. A partir de 1990, le virus DEN 2 était présent également dans l'intérieur du pays et en {A}mazonie. A {R}io de {J}aneiro (1990-91) et dans l'{E}tat du {C}eara (1994) où les deux sérotypes DEN 1 et DEN 2 circulaient en même temps, plusieurs cas de DHS/DSS ont été signalés. {E}nviron 500000 cas de {D}engue ont été notifiés de 1982 à 1994. {A}edes aegypti est le seul vecteur urbain à partir duquel 4 souches de DEN 4, 7 souches de DEN 1 et 16 souches de DEN 2 ont été isolées. {L}a transmission transovarienne ne semble pas avoir lieu chez cette espèce au {B}résil.}}, 651 keywords = {{D}engue 1; {D}engue 2; {D}engue 4; {A}edes aegypti; {A}edes albopictus; {B}résil; histoire; epidémiologie}, 652 language = {{F}rançais}, 653 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratorio de {A}rbovirus , {U}nité de recherches en virologie , {I}nstitut {E}vandro {C}hagas-FNS}, 657 654 pages = {128-136}, 658 journal = { Bulletin de la Soci{\'e}t{\'e}de pathologie exotique (1990)},655 journal = {{B}ulletin de la {S}ociété de pathologie exotique (1990)}, 659 656 volume = {89}, 660 657 audience = {internationale}, … … 668 665 timestamp={20121014}, 669 666 title = {{Ocean biogeochemistry exhibits contrasting responses to a large scale reduction in dust deposition}}, 670 author = { A. Tagliabue and Laurent Bopp and Olivier Aumont},671 abstract = {{Dust deposition of iron is thought to be an important control on ocean biogeochemistry and air-sea CO2 exchange. In this study, we examine the impact of a large scale, yet climatically realistic, reduction in the aeolian Fe input during a 240 year transient simulation. In contrast to previous studies, we find that the ocean biogeochemical cycles of carbon and nitrogen are relatively insensitive (globally) to a 60\% reduction in Fe input from dust. Net primary productivity (NPP) is reduced in the Fe limited regions, but the excess macronutrients that result are able to fuel additional NPP elsewhere. Overall, NPP and air-sea CO2 exchange are only reduced by around 3\% between 1860 and 2100. While the nitrogen cycle is perturbed more significantly (by \~15\%), reduced N2 fixation is balanced by a concomitant decline in denitrification. Feedbacks between N2 fixation and denitrification are controlled by variability in surface utilization of inorganic nitrogen and subsurface oxygen consumption, as well as the direct influence of Fe on N2 fixation. Overall, there is relatively little impact of reduced aeolian Fe input (}},672 language = { Anglais},673 affiliation = { Laboratoire des sciences du climat et de l'environnement - LSCE , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},667 author = {{A}. {T}agliabue and {L}aurent {B}opp and {O}livier {A}umont}, 668 abstract = {{Dust deposition of iron is thought to be an important control on ocean biogeochemistry and air-sea CO2 exchange. {I}n this study, we examine the impact of a large scale, yet climatically realistic, reduction in the aeolian {F}e input during a 240 year transient simulation. {I}n contrast to previous studies, we find that the ocean biogeochemical cycles of carbon and nitrogen are relatively insensitive (globally) to a 60\% reduction in {F}e input from dust. {N}et primary productivity (NPP) is reduced in the {F}e limited regions, but the excess macronutrients that result are able to fuel additional NPP elsewhere. {O}verall, NPP and air-sea CO2 exchange are only reduced by around 3\% between 1860 and 2100. {W}hile the nitrogen cycle is perturbed more significantly (by \~15\%), reduced N2 fixation is balanced by a concomitant decline in denitrification. {F}eedbacks between N2 fixation and denitrification are controlled by variability in surface utilization of inorganic nitrogen and subsurface oxygen consumption, as well as the direct influence of {F}e on N2 fixation. {O}verall, there is relatively little impact of reduced aeolian {F}e input (}}, 669 language = {{A}nglais}, 670 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 674 671 pages = {11-24}, 675 journal = { Biogeosciences},672 journal = {{B}iogeosciences}, 676 673 volume = {5}, 677 674 number = {1}, … … 688 685 timestamp={20121014}, 689 686 title = {{Why climate sensitivity may not be so unpredictable ?}}, 690 author = { Alexis Hannart and Jean-Louis Dufresne and Philipe Naveau},691 abstract = {{Different explanations have been proposed as to why the range of climate sensitivity predicted by GCMs have not lessened substantially in the last decades, and subsequently if it can be reduced. One such study (\textit{Why is climate sensitivity so unpredictable?}, \cite{RB07}) adressed these questions using rather simple theoretical considerations and reached the conclusion that reducing uncertainties on climate feedbacks and underlying climate processes will not yield a large reduction in the envelope of climate sensitivity. In this letter, we revisit the premises of this conclusion. We show that it results from a mathematical artefact caused by peculiar definitions of uncertainty used by these authors. Applying standard concepts and definitions of descriptive statistics to the exact same framework of analysis as Roe and Baker, we show that within this simple framework, reducing inter-model spread on feedbacks does in fact induce a reduction of uncertainty on climate sensitivity, almost proportionally. Therefore, following Roe and Baker assumptions, climate sensitivity is actually not so unpredictable. \%We then briefly focus on ongoing advances in cloud physics that may narrow the spread on feedbacks, thus reducing the uncertainty on climate sensitivity.}},692 language = { Anglais},693 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD , Laboratoire des sciences du climat et de l'environnement - LSCE},687 author = {{A}lexis {H}annart and {J}ean-{L}ouis {D}ufresne and {P}hilipe {N}aveau}, 688 abstract = {{Different explanations have been proposed as to why the range of climate sensitivity predicted by GCMs have not lessened substantially in the last decades, and subsequently if it can be reduced. {O}ne such study (\textit{Why is climate sensitivity so unpredictable?}, \cite{RB07}) adressed these questions using rather simple theoretical considerations and reached the conclusion that reducing uncertainties on climate feedbacks and underlying climate processes will not yield a large reduction in the envelope of climate sensitivity. {I}n this letter, we revisit the premises of this conclusion. {W}e show that it results from a mathematical artefact caused by peculiar definitions of uncertainty used by these authors. {A}pplying standard concepts and definitions of descriptive statistics to the exact same framework of analysis as {R}oe and {B}aker, we show that within this simple framework, reducing inter-model spread on feedbacks does in fact induce a reduction of uncertainty on climate sensitivity, almost proportionally. {T}herefore, following {R}oe and {B}aker assumptions, climate sensitivity is actually not so unpredictable. \%We then briefly focus on ongoing advances in cloud physics that may narrow the spread on feedbacks, thus reducing the uncertainty on climate sensitivity.}}, 689 language = {{A}nglais}, 690 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire de {M}étéorologie {D}ynamique - LMD , {L}aboratoire des sciences du climat et de l'environnement - LSCE}, 694 691 pages = {L16707}, 695 journal = { Geophysical Research Letters},692 journal = {{G}eophysical {R}esearch {L}etters}, 696 693 volume = {36}, 697 694 audience = {internationale}, … … 705 702 loceanbibid = {01870}, 706 703 timestamp={20121014}, 707 title = {{Arboviroses {\'e}mergentes au Br{\'e}sil}},708 author = { Nicolas Dégallier and A. P. De Andrade Travassos Da Rosa and P. De Tarso Ribeiro Vilarinhos},709 language = { Fran{\c c}ais},710 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},711 booktitle = {{Recherches de l'IRD au Br{\'e}sil depuis 1998}},712 publisher = { Charbel Gr{\'a}fica Editora, Bras{\'\i}lia, Br{\'e}sil},704 title = {{Arboviroses émergentes au {B}résil}}, 705 author = {{N}icolas {D}égallier and A. P. {D}e {A}ndrade {T}ravassos {D}a {R}osa and P. {D}e {T}arso {R}ibeiro {V}ilarinhos}, 706 language = {{F}rançais}, 707 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 708 booktitle = {{Recherches de l'IRD au {B}résil depuis 1998}}, 709 publisher = {{C}harbel {G}ráfica {E}ditora, {B}rasília, {B}résil}, 713 710 pages = {102-104}, 714 editor = { P. Sabat{\'e} \& C.Boutrolle},711 editor = {{P}. {S}abaté \& C. Boutrolle}, 715 712 year = {2006}, 716 713 comment = {20121114 : ++ compléter prénom et diacritique dans nom dans hal}, … … 721 718 loceanbibid = {01869}, 722 719 timestamp={20121014}, 723 title = {{Col {\'e}opt{\`e}res histeridae de Guyane fran{\c c}aise...}},724 author = { Nicolas D{\'e}gallier},725 language = { Anglais},726 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},727 booktitle = {{Insectes de Guyane : beaut{\'e} et diversit{\'e}}},720 title = {{Coléoptères histeridae de {G}uyane française...}}, 721 author = {{N}icolas {D}égallier}, 722 language = {{A}nglais}, 723 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 724 booktitle = {{Insectes de {G}uyane : beauté et diversité}}, 728 725 publisher = {SEPANGUY}, 729 726 pages = {67-74}, 730 editor = { Suzanon C.},727 editor = {{S}uzanon C.}, 731 728 year = {2004}, 732 729 } … … 736 733 loceanbibid = {01868}, 737 734 timestamp={20121014}, 738 title = {{Distribution of larval Krefftichthys anderssoni (Myctophidae, Pisces) at the Kerguelen Archipelago (Southern Indian Ocean) modelled using GIS and habitat suitability}},739 author = { P. Koubbi and G. Duhamel and X. Harlay and P.D. Eastwood and I. Durand and Y.-H. Park},740 language = { Anglais},741 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},735 title = {{Distribution of larval {K}refftichthys anderssoni (Myctophidae, {P}isces) at the {K}erguelen {A}rchipelago (Southern {I}ndian {O}cean) modelled using GIS and habitat suitability}}, 736 author = {{P}. {K}oubbi and G. {D}uhamel and X. {H}arlay and P.D. {E}astwood and I. {D}urand and {Y}oung-{H}yang {P}ark}, 737 language = {{A}nglais}, 738 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 742 739 booktitle = {{Antarctic biology in a global context}}, 743 publisher = { Backhuys Publishers, Leiden},740 publisher = {{B}ackhuys {P}ublishers, {L}eiden}, 744 741 pages = {215-223}, 745 editor = {A.H.L. Huiskes and W.W.C. Gieskes and J. Rozema and R.M.L. Schornoa and S.M. van der Vies and W.J Wolf},742 editor = {A.H.L. {H}uiskes and W.W.C. {G}ieskes and J. {R}ozema and R.M.L. {S}chornoa and S.M. van der {V}ies and W.J {W}olf}, 746 743 series = {ISBN 90 5782 0879 X}, 747 744 year = {2003}, … … 754 751 timestamp={20121014}, 755 752 title = {{Response of diatoms distribution to global warming and potential implications: A global model study}}, 756 author = { Laurent Bopp and Olivier Aumont and Patricia Cadule and S. Alvain and M. Gehlen},757 language = { Anglais},758 affiliation = { Laboratoire des sciences du climat et de l'environnement - LSCE , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Institut Pierre-Simon-Laplace - IPSL},753 author = {{L}aurent {B}opp and {O}livier {A}umont and {P}atricia {C}adule and S. {A}lvain and M. {G}ehlen}, 754 language = {{A}nglais}, 755 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL}, 759 756 pages = {doi:10.1029/2005GL023653}, 760 journal = { Geophysical Research Letters},757 journal = {{G}eophysical {R}esearch {L}etters}, 761 758 volume = {32}, 762 audience = {non sp {\'e}cifi{\'e}e},759 audience = {non spécifiée}, 763 760 year = {2005}, 764 761 } … … 769 766 timestamp={20121014}, 770 767 title = {{On the origin of the 100-kyr cycle in the astronomical forcing}}, 771 author = { André Berger and Marie-France Loutre and Jean-Luc Mélice},772 language = { Anglais},773 affiliation = { Institut d'Astronomie et de G{\'e}ophysique G. Lema{\^\i}tre - UCL-ASTR , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Oceanography Department - UCT-OD},768 author = {{A}ndré {B}erger and {M}arie-{F}rance {L}outre and {J}ean-{L}uc {M}élice}, 769 language = {{A}nglais}, 770 affiliation = {{I}nstitut d'{A}stronomie et de {G}éophysique G. {L}emaître - UCL-ASTR , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {O}ceanography {D}epartment - UCT-OD}, 774 771 pages = {doi:10.1029/2005PA001173}, 775 772 journal = {PALEOCEANOGRAPHY}, 776 773 volume = {20}, 777 audience = {non sp {\'e}cifi{\'e}e},774 audience = {non spécifiée}, 778 775 doi = {10.1029/2005PA001173}, 779 776 year = {2005}, … … 785 782 timestamp={20121014}, 786 783 title = {{Role of cyanobacteria in the biodegradation of crude oil by a tropical cyanobacterial mat}}, 787 author = { F. Chaillan and M. Gugger and Alain Saliot and A. Couté and J. Oudot},788 language = { Anglais},789 affiliation = { Ecosyst{\`e}mes et Interactions Toxiques , Laboratoire de biog{\'e}ochimie et chimie marines - LBCM},784 author = {{F}. {C}haillan and M. {G}ugger and {A}lain {S}aliot and A. {C}outé and J. {O}udot}, 785 language = {{A}nglais}, 786 affiliation = {{E}cosystèmes et {I}nteractions {T}oxiques , {L}aboratoire de biogéochimie et chimie marines - LBCM}, 790 787 pages = {1574-1582}, 791 journal = { Chemosphere},788 journal = {{C}hemosphere}, 792 789 volume = {62}, 793 audience = {non sp {\'e}cifi{\'e}e},790 audience = {non spécifiée}, 794 791 doi = {10.1016/j.chemosphere.2005.06.050}, 795 792 year = {2006}, … … 801 798 loceanbibid = {01864}, 802 799 timestamp={20121014}, 803 title = {{Escutar o r {\'a}dio aumenta o risco de ser picado por mosquitos?}},804 author = { Nicolas Degallier and Hamilton Antonio De Oliveira Monteiro and Francisco Corrêa Castro and Orlando Vaz Da Silva and Hélio Augusto Cardoso Saraiva and Roberto Carlos Feitosa Brandão and Miguel Moyses Alvão},805 language = { Portugais},806 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laborat{\'o}rio de Arbov{\'\i}rus - LA},800 title = {{Escutar o rádio aumenta o risco de ser picado por mosquitos?}}, 801 author = {{N}icolas {D}égallier and {H}amilton {A}ntonio {D}e {O}liveira {M}onteiro and {F}rancisco {C}orrêa {C}astro and {O}rlando {V}az {D}a {S}ilva and {H}élio {A}ugusto {C}ardoso {S}araiva and {R}oberto {C}arlos {F}eitosa {B}randão and {M}iguel {M}oyses {A}lvão}, 802 language = {{P}ortugais}, 803 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratório de {A}rbovìrus - LA}, 807 804 pages = {685-686}, 808 journal = { Revista de Sa{\'u}de P{\'u}blica},805 journal = {{R}evista de {S}aúde Pública}, 809 806 volume = {39}, 810 audience = {non sp {\'e}cifi{\'e}e},807 audience = {non spécifiée}, 811 808 doi = {10.1590/S0034-89102005000400026}, 812 809 year = {2005}, … … 818 815 loceanbibid = {01863}, 819 816 timestamp={20121014}, 820 title = {{Variability of the throughflow at its exit in the Indian Ocean}},821 author = { Michèle Fieux and Robert Molcard and R. Morrow and Annie Kartavtseff and A. G. Ilahude},822 language = { Anglais},823 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS , Puslitbang Oseanologi - PO},817 title = {{Variability of the throughflow at its exit in the {I}ndian {O}cean}}, 818 author = {{M}ichèle {F}ieux and {R}obert {M}olcard and R. {M}orrow and {A}nnie {K}artavtseff and A. G. {I}lahude}, 819 language = {{A}nglais}, 820 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire d'études en {G}éophysique et océanographie spatiales - LEGOS , {P}uslitbang {O}seanologi - PO}, 824 821 pages = {L14616}, 825 journal = { Geophysical Research Letters},822 journal = {{G}eophysical {R}esearch {L}etters}, 826 823 volume = {32}, 827 audience = {non sp {\'e}cifi{\'e}e},824 audience = {non spécifiée}, 828 825 doi = {10.1029/2005GL022836}, 829 826 year = {2005}, … … 836 833 timestamp={20121014}, 837 834 title = {{Internal gravity waves in a dipolar wind: a wave--vortex interaction experiment in a stratified fluid}}, 838 author = { Ramiro Godoy-Diana and Jean-Marc Chomaz and Claire Donnadieu},839 language = { Anglais},840 affiliation = { Laboratoire d'hydrodynamique - LadHyX , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},835 author = {{R}amiro {G}odoy-{D}iana and {J}ean-{M}arc {C}homaz and {C}laire {D}onnadieu}, 836 language = {{A}nglais}, 837 affiliation = {{L}aboratoire d'hydrodynamique - {L}adHyX , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 841 838 pages = {281-308}, 842 journal = { Journal of Fluid Mechanics},839 journal = {{J}ournal of {F}luid {M}echanics}, 843 840 volume = {548}, 844 audience = {non sp {\'e}cifi{\'e}e},841 audience = {non spécifiée}, 845 842 doi = {10.1017/S0022112005007536}, 846 843 year = {2006}, … … 852 849 timestamp={20121014}, 853 850 title = {{Ecosystem dynamics based on plankton functional types for global ocean biogeochemistry models}}, 854 author = { Corinne Le Quéré and Sandy P. Harrison and I. Colin Prentice and Erik T. Buitenhuis and Olivier Aumont and Laurent Bopp and Hervé Claustre and Leticia Cotrim Da Cunha and Richard Geider and Xavier Giraud and Christine Klaas and Karen E. Kohfeld and Louis Legendre and Manfredi Manizza and Trevor Platt and Richard B. Rivkin and Shubha Sathyendranath and Julia Uitz and Andy J. Watson and Dieter Wolf-Gladrow},855 language = { Anglais},856 affiliation = { Max-Planck-Institut f{\"u}r Biogeochemie Jena (MPI BGC) - MPI BGC , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire des sciences du climat et de l'environnement - LSCE , Laboratoire d'oc{\'e}anographie de Villefranche - LOV , Department of Biological Sciences - BS , School of Geographical Sciences , Department of Oceanography - DO , Ocean Sciences Centre - OSC},851 author = {{C}orinne {L}e {Q}uéré and {S}andy P. {H}arrison and I. {C}olin {P}rentice and {E}rik T. {B}uitenhuis and {O}livier {A}umont and {L}aurent {B}opp and {H}ervé {C}laustre and {L}eticia {C}otrim {D}a {C}unha and {R}ichard {G}eider and {X}avier {G}iraud and {C}hristine {K}laas and {K}aren E. {K}ohfeld and {L}ouis {L}egendre and {M}anfredi {M}anizza and {T}revor {P}latt and {R}ichard B. {R}ivkin and {S}hubha {S}athyendranath and {J}ulia {U}itz and {A}ndy J. {W}atson and {D}ieter {W}olf-{G}ladrow}, 852 language = {{A}nglais}, 853 affiliation = {{M}ax-{P}lanck-{I}nstitut für {B}iogeochemie {J}ena (MPI BGC) - MPI BGC , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'océanographie de {V}illefranche - LOV , {D}epartment of {B}iological {S}ciences - BS , {S}chool of {G}eographical {S}ciences , {D}epartment of {O}ceanography - DO , {O}cean {S}ciences {C}entre - OSC}, 857 854 pages = {2016-2040}, 858 journal = { Global Change Biology},855 journal = {{G}lobal {C}hange {B}iology}, 859 856 volume = {11(11)}, 860 note = {article de base pour un mod {\`e}le avec bact{\'e}ries, picoautotrophes, fixateurs d'azote, de calcaire, diatom{\'e}es, producteurs de DMS, divers phyto, micro, meso et macroplancton},861 audience = {non sp {\'e}cifi{\'e}e},857 note = {article de base pour un modèle avec bactéries, picoautotrophes, fixateurs d'azote, de calcaire, diatomées, producteurs de DMS, divers phyto, micro, meso et macroplancton}, 858 audience = {non spécifiée}, 862 859 doi = {10.1111/j.1365-2486.2005.1004.x}, 863 860 year = {2005}, … … 868 865 loceanbibid = {01860}, 869 866 timestamp={20121014}, 870 title = {{Alkenone and coccolith records of the mid- Pleistocene in the south-east Atlantic: Implications for the Uk'37 index and South African climate}},871 author = { Erin L. McClymont and Antoni Rosell-Melé and Jacques Giraudeau and Catherine Pierre and Jerry M. Lloyd},872 language = { Anglais},873 affiliation = { Department of Geography , ICREA and ICTA , Environnements et Pal{\'e}oenvironnements OC{\'e}aniques - EPOC , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},867 title = {{Alkenone and coccolith records of the mid-{P}leistocene in the south-east {A}tlantic: {I}mplications for the {U}k'37 index and {S}outh {A}frican climate}}, 868 author = {{E}rin L. {M}cClymont and {A}ntoni {R}osell-{M}elé and {J}acques {G}iraudeau and {C}atherine {P}ierre and {J}erry M. {L}loyd}, 869 language = {{A}nglais}, 870 affiliation = {{D}epartment of {G}eography , ICREA and ICTA , {E}nvironnements et {P}aléoenvironnements OCéaniques - EPOC , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 874 871 pages = {1559-1572}, 875 journal = { Quaternary Science Reviews},872 journal = {{Q}uaternary {S}cience {R}eviews}, 876 873 volume = {24(14-15)}, 877 audience = {non sp {\'e}cifi{\'e}e},874 audience = {non spécifiée}, 878 875 doi = {10.1016/j.quascirev.2004.06.024}, 879 876 year = {2005}, … … 886 883 timestamp={20121014}, 887 884 title = {{Polar lipid biomarkers of free-living bacteria from oligotrophic marine waters}}, 888 author = { Laurence Méjanelle and Jeanne Laureillard and Fereidoun Rassoulzadegan},889 language = { Anglais},890 affiliation = { Laboratoire de biog{\'e}ochimie et chimie marines - LBCM , Observatoire oc{\'e}anologique de Villefranche-sur-mer - OOVM},885 author = {{L}aurence {M}éjanelle and {J}eanne {L}aureillard and {F}ereidoun {R}assoulzadegan}, 886 language = {{A}nglais}, 887 affiliation = {{L}aboratoire de biogéochimie et chimie marines - LBCM , {O}bservatoire océanologique de {V}illefranche-sur-mer - OOVM}, 891 888 pages = {365-383}, 892 journal = { Biogeochemistry},889 journal = {{B}iogeochemistry}, 893 890 volume = {72(3)}, 894 audience = {non sp {\'e}cifi{\'e}e},891 audience = {non spécifiée}, 895 892 doi = {10.1007/s10533-004-0374-9}, 896 893 year = {2005}, … … 902 899 loceanbibid = {01858}, 903 900 timestamp={20121014}, 904 title = {{Evidence for the Antarctic circumpolar wave in the sub-Antarctic during the past 50 years}},905 author = { Jean-Luc Mélice and J.R.E. Lutjeharms and H. Goosse and T. Fichefet and C. J. C. Reason},906 language = { Anglais},907 affiliation = { Department of Oceanography , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Institut d'Astronomie et de G{\'e}ophysique G. Lema{\^\i}tre},901 title = {{Evidence for the {A}ntarctic circumpolar wave in the sub-{A}ntarctic during the past 50 years}}, 902 author = {{J}ean-{L}uc {M}élice and J.R.E. {L}utjeharms and H. {G}oosse and T. {F}ichefet and C. J. C. {R}eason}, 903 language = {{A}nglais}, 904 affiliation = {{D}epartment of {O}ceanography , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {I}nstitut d'{A}stronomie et de {G}éophysique G. {L}emaître}, 908 905 pages = {L14614}, 909 journal = { Geophysical Research Letters},906 journal = {{G}eophysical {R}esearch {L}etters}, 910 907 volume = {32}, 911 audience = {non sp {\'e}cifi{\'e}e},908 audience = {non spécifiée}, 912 909 doi = {10.1029/2005GL023361}, 913 910 year = {2005}, … … 919 916 loceanbibid = {01857}, 920 917 timestamp={20121014}, 921 title = {{Diversity of Bacteria and Archaea associated with a carbonate-rich metalliferous sediment sample from the Rainbow vent field on the Mid-Atlantic Ridge}},922 author = { Olivier Nercessian and Yves Fouquet and Catherine Pierre and Daniel Prieur and Christian Jeanthon},923 language = { Anglais},924 affiliation = { Laboratoire des Sciences de l'Environnement Marin - LEMAR , D{\'e}partement G{\'e}osciences Marines , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},918 title = {{Diversity of {B}acteria and {A}rchaea associated with a carbonate-rich metalliferous sediment sample from the {R}ainbow vent field on the {M}id-{A}tlantic {R}idge}}, 919 author = {{O}livier {N}ercessian and {Y}ves {F}ouquet and {C}atherine {P}ierre and {D}aniel {P}rieur and {C}hristian {J}eanthon}, 920 language = {{A}nglais}, 921 affiliation = {{L}aboratoire des {S}ciences de l'{E}nvironnement {M}arin - LEMAR , {D}épartement {G}éosciences {M}arines , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 925 922 pages = {698-714}, 926 journal = { Environmental microbiology},923 journal = {{E}nvironmental microbiology}, 927 924 volume = {7(5)}, 928 audience = {non sp {\'e}cifi{\'e}e},925 audience = {non spécifiée}, 929 926 doi = {10.1111/j.1462-2920.2005.00744.x}, 930 927 year = {2005}, … … 936 933 timestamp={20121014}, 937 934 title = {{Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms}}, 938 author = { James C. Orr and Victoria J. Fabry and Olivier Aumont and Laurent Bopp and Scott C. Doney and Richard A. Feely and Anand Gnanadesikan and Nicolas Gruber and Akio Ishida and Fortunat Joos and Robert M. Key and Keith Lindsay and Ernst Maier-Reimer and Richard J. Matear and Patrick Monfray and Anne Mouchet and Raymond G. Najjar and Gian-Kasper Plattner and Keith B. Rodgers and Christopher L. Sabine and Jorge L. Sarmiento and Reiner Schlitzer and Richard D. Slater and Ian J. Totterdell and Marie-France Weirig and Yasuhiro Yamanaka and Andrew Yool},939 language = { Anglais},940 affiliation = { Laboratoire des sciences du climat et de l'environnement - LSCE , Department of Biological Sciences , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Woods Hole Oceanographic Institution , Pacific Marine Environmental Laboratory , Geophysical Fluid Dynamics Laboratory , Institute of Geophysics and Planetary Physics [Los Angeles] - IGPP , Frontier Research Center for Global Change , Climate and Environmental Physics, Physics Institute , Atmospheric and Oceanic Sciences (AOS) Program , National Center for Atmospheric Research - NCAR , Max Planck Institut f{\"u}r Meteorologie , Marine Research and Antarctic Climate and Ecosystems CRC , Astrophysics and Geophysics Institute , Department of Meteorology, Pennsylvania State University , Department of Bentho-pelagic processes , National Oceanography Centre Southampton},935 author = {{J}ames C. {O}rr and {V}ictoria J. {F}abry and {O}livier {A}umont and {L}aurent {B}opp and {S}cott C. {D}oney and {R}ichard A. {F}eely and {A}nand {G}nanadesikan and {N}icolas {G}ruber and {A}kio {I}shida and {F}ortunat {J}oos and {R}obert M. {K}ey and {K}eith {L}indsay and {E}rnst {M}aier-{R}eimer and {R}ichard J. {M}atear and {P}atrick {M}onfray and {A}nne {M}ouchet and {R}aymond G. {N}ajjar and {G}ian-{K}asper {P}lattner and {K}eith B. {R}odgers and {C}hristopher L. {S}abine and {J}orge L. {S}armiento and {R}einer {S}chlitzer and {R}ichard D. {S}later and {I}an J. {T}otterdell and {M}arie-{F}rance {W}eirig and {Y}asuhiro {Y}amanaka and {A}ndrew {Y}ool}, 936 language = {{A}nglais}, 937 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {D}epartment of {B}iological {S}ciences , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {W}oods {H}ole {O}ceanographic {I}nstitution , {P}acific {M}arine {E}nvironmental {L}aboratory , {G}eophysical {F}luid {D}ynamics {L}aboratory , {I}nstitute of {G}eophysics and {P}lanetary {P}hysics [Los {A}ngeles] - IGPP , {F}rontier {R}esearch {C}enter for {G}lobal {C}hange , {C}limate and {E}nvironmental {P}hysics, {P}hysics {I}nstitute , {A}tmospheric and {O}ceanic {S}ciences (AOS) {P}rogram , {N}ational {C}enter for {A}tmospheric {R}esearch - NCAR , {M}ax {P}lanck {I}nstitut für {M}eteorologie , {M}arine {R}esearch and {A}ntarctic {C}limate and {E}cosystems CRC , {A}strophysics and {G}eophysics {I}nstitute , {D}epartment of {M}eteorology, {P}ennsylvania {S}tate {U}niversity , {D}epartment of {B}entho-pelagic processes , {N}ational {O}ceanography {C}entre {S}outhampton}, 941 938 pages = {681-686}, 942 journal = { Nature},939 journal = {{N}ature}, 943 940 volume = {437}, 944 audience = {non sp {\'e}cifi{\'e}e},941 audience = {non spécifiée}, 945 942 doi = {10.1038/nature04095}, 946 943 year = {2005}, … … 951 948 loceanbibid = {01855}, 952 949 timestamp={20121014}, 953 title = {{Climate variability at Marion Island, Southern Ocean, since 1960}},954 author = { Mathieu Rouault and Jean-Luc Mélice and Chris J. C. Reason and Johann R. E. Lutjeharms},955 language = { Anglais},956 affiliation = { Department of Oceanography , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},950 title = {{Climate variability at {M}arion {I}sland, {S}outhern {O}cean, since 1960}}, 951 author = {{M}athieu {R}ouault and {J}ean-{L}uc {M}élice and {C}hris J. C. {R}eason and {J}ohann R. E. {L}utjeharms}, 952 language = {{A}nglais}, 953 affiliation = {{D}epartment of {O}ceanography , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 957 954 pages = {C05007}, 958 journal = { Journal of Geophysical Research},955 journal = {{J}ournal of {G}eophysical {R}esearch}, 959 956 volume = {110}, 960 audience = {non sp {\'e}cifi{\'e}e},957 audience = {non spécifiée}, 961 958 doi = {10.1029/2004JC002492}, 962 959 year = {2005}, … … 967 964 loceanbibid = {01854}, 968 965 timestamp={20121014}, 969 title = {{Causes of large-scale sea level variations in the Southern Ocean: Analyses of sea level and a barotropic model}},970 author = { Frédéric Vivier and Kathryn A. Kelly and Migel Harismendy},971 language = { Anglais},972 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},966 title = {{Causes of large-scale sea level variations in the {S}outhern {O}cean: {A}nalyses of sea level and a barotropic model}}, 967 author = {{F}rédéric {V}ivier and {K}athryn A. {K}elly and {M}igel {H}arismendy}, 968 language = {{A}nglais}, 969 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 973 970 pages = {C09014}, 974 journal = { Journal of Geophysical Research},971 journal = {{J}ournal of {G}eophysical {R}esearch}, 975 972 volume = {110}, 976 audience = {non sp {\'e}cifi{\'e}e},973 audience = {non spécifiée}, 977 974 doi = {10.1029/2004JC002773}, 978 975 year = {2005}, … … 983 980 loceanbibid = {01853}, 984 981 timestamp={20121014}, 985 title = {{Adjustment of near-equatorial wind stress with four-dimensional variational data assimilation in a model of the Pacific Ocean}},986 author = { Femke C. Vossepoel and Anthony T. Weaver and Jérôme Vialard and Pascale Delecluse},987 language = { Anglais},988 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Centre Europ{\'e}en de Recherche et de Formation Avanc{\'e}e en Calcul Scientifique - CERFACS},982 title = {{Adjustment of near-equatorial wind stress with four-dimensional variational data assimilation in a model of the {P}acific {O}cean}}, 983 author = {{F}emke C. {V}ossepoel and {A}nthony T. {W}eaver and {J}érôme {V}ialard and {P}ascale {D}elecluse}, 984 language = {{A}nglais}, 985 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {C}entre {E}uropéen de {R}echerche et de {F}ormation {A}vancée en {C}alcul {S}cientifique - CERFACS}, 989 986 pages = {2070-2083}, 990 journal = { Monthly Weather Review},987 journal = {{M}onthly {W}eather {R}eview}, 991 988 volume = {132(8)}, 992 audience = {non sp {\'e}cifi{\'e}e},989 audience = {non spécifiée}, 993 990 doi = {10.1175/1520-0493}, 994 991 year = {2004}, … … 1000 997 timestamp={20121014}, 1001 998 title = {{Globalizing results from ocean in situ iron fertilization studies}}, 1002 author = { Olivier Aumont and Laurent Bopp},1003 language = { Anglais},1004 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire des sciences du climat et de l'environnement - LSCE},999 author = {{O}livier {A}umont and {L}aurent {B}opp}, 1000 language = {{A}nglais}, 1001 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire des sciences du climat et de l'environnement - LSCE}, 1005 1002 pages = {GB2017}, 1006 journal = { Global Biogeochem. Cycles},1003 journal = {{G}lobal {B}iogeochem. {C}ycles}, 1007 1004 volume = {20(2)}, 1008 1005 note = {http://www.agu.org/journals/gb/gb0602/2005GB002591/}, 1009 audience = {non sp {\'e}cifi{\'e}e},1006 audience = {non spécifiée}, 1010 1007 doi = {10.1029/2005GB002591}, 1011 1008 year = {2006}, … … 1017 1014 timestamp={20121014}, 1018 1015 title = {{Biogeochemical fluxes through mesozooplankton}}, 1019 author = { E. Buitenhuis and C. Le Quéré and Olivier Aumont and G. Beaugrand and A. Bunker and A. Hirst and T. Ikeda and T. O'Brien and S. Piontkovski and D. Straile},1020 language = { Anglais},1021 affiliation = { Max Planck Institute for Biogeochemistry , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Sir Alister Hardy Foundation for Ocean Science - SAHFOS , Heriot-Watt University , British Antarctic Survey - BAS , Plankton Laboratory, Graduate School of Fisheries Sciences, , National Marine Fisheries Service , Marine Sciences Research Center , Limnological Institute},1016 author = {{E}. {B}uitenhuis and C. {L}e {Q}uéré and {O}livier {A}umont and G. {B}eaugrand and A. {B}unker and A. {H}irst and T. {I}keda and T. O'{B}rien and S. {P}iontkovski and D. {S}traile}, 1017 language = {{A}nglais}, 1018 affiliation = {{M}ax {P}lanck {I}nstitute for {B}iogeochemistry , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {S}ir {A}lister {H}ardy {F}oundation for {O}cean {S}cience - SAHFOS , {H}eriot-{W}att {U}niversity , {B}ritish {A}ntarctic {S}urvey - BAS , {P}lankton {L}aboratory, {G}raduate {S}chool of {F}isheries {S}ciences, , {N}ational {M}arine {F}isheries {S}ervice , {M}arine {S}ciences {R}esearch {C}enter , {L}imnological {I}nstitute}, 1022 1019 pages = {GB2003}, 1023 journal = { Global Biogeochemical Cycles},1020 journal = {{G}lobal {B}iogeochemical {C}ycles}, 1024 1021 volume = {20}, 1025 1022 note = {http://www.agu.org/journals/gb/gb0602/2005GB002511/}, 1026 audience = {non sp {\'e}cifi{\'e}e},1023 audience = {non spécifiée}, 1027 1024 doi = {10.1029/2005GB002511}, 1028 1025 year = {2006}, … … 1034 1031 timestamp={20121014}, 1035 1032 title = {{Impact of sub-mesoscale physics on production and subduction of phytoplankton in an oligotrophic regime}}, 1036 author = { Marina Lévy and Patrice Klein and Anne-Marie Tréguier},1037 language = { Anglais},1038 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1033 author = {{M}arina {L}évy and {P}atrice {K}lein and {A}nne-{M}arie {T}réguier}, 1034 language = {{A}nglais}, 1035 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1039 1036 pages = {535-565}, 1040 journal = { J. Mar. Res},1037 journal = {{J}. {M}ar. {R}es}, 1041 1038 volume = {59}, 1042 1039 number = {4}, 1043 audience = {non sp {\'e}cifi{\'e}e},1040 audience = {non spécifiée}, 1044 1041 year = {2001}, 1045 1042 comment = {20121114 : ++ compléter prénom dans hal}, … … 1051 1048 loceanbibid = {01849}, 1052 1049 timestamp={20121014}, 1053 title = {{Mesoscale variability of phytoplankton and of new production : Impact of the large scale nutrient distribution}},1054 author = { Marina Lévy},1055 language = { Anglais},1056 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1050 title = {{Mesoscale variability of phytoplankton and of new production : {I}mpact of the large scale nutrient distribution}}, 1051 author = {{M}arina {L}évy}, 1052 language = {{A}nglais}, 1053 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1057 1054 pages = {3358}, 1058 journal = { Journal of Geophysical Research},1055 journal = {{J}ournal of {G}eophysical {R}esearch}, 1059 1056 volume = {108}, 1060 1057 number = {C11}, 1061 1058 note = {http://www.agu.org/pubs/crossref/2003/2002JC001577.shtml}, 1062 audience = {non sp {\'e}cifi{\'e}e},1059 audience = {non spécifiée}, 1063 1060 doi = {10.1029/2002JC001577}, 1064 1061 year = {2003}, … … 1070 1067 loceanbibid = {01848}, 1071 1068 timestamp={20121014}, 1072 title = {{Comparing the results of a 4D-variational assimilation of satellite and in situ data with WOCE CITHER hydrographic measurements in the tropical Atlantic}},1073 author = { E. Greiner and Sabine Arnault},1074 language = { Anglais},1075 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1069 title = {{Comparing the results of a 4D-variational assimilation of satellite and in situ data with WOCE CITHER hydrographic measurements in the tropical {A}tlantic}}, 1070 author = {{E}. {G}reiner and {S}abine {A}rnault}, 1071 language = {{A}nglais}, 1072 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1076 1073 pages = {1-68}, 1077 journal = { Progress In Oceanography},1074 journal = {{P}rogress {I}n {O}ceanography}, 1078 1075 volume = {47}, 1079 1076 number = {1}, 1080 audience = {non sp {\'e}cifi{\'e}e},1077 audience = {non spécifiée}, 1081 1078 doi = {10.1016/S0079-6611(00)00031-8}, 1082 1079 year = {2000}, … … 1088 1085 loceanbibid = {01847}, 1089 1086 timestamp={20121014}, 1090 title = {{Twelve monthly experiments of 4D-variational assimilation in the tropical Atlantic during 1987. Part 1: Method and statistical results}},1091 author = { E. Greiner and Sabine Arnault and A. Morlière},1092 language = { Anglais},1093 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1087 title = {{Twelve monthly experiments of 4D-variational assimilation in the tropical {A}tlantic during 1987. {P}art 1: {M}ethod and statistical results}}, 1088 author = {{E}. {G}reiner and {S}abine {A}rnault and A. {M}orlière}, 1089 language = {{A}nglais}, 1090 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1094 1091 pages = {141-202}, 1095 journal = { Prog. Oceanogr.},1092 journal = {{P}rog. {O}ceanogr.}, 1096 1093 volume = {41}, 1097 1094 number = {2}, 1098 audience = {non sp {\'e}cifi{\'e}e},1095 audience = {non spécifiée}, 1099 1096 doi = {10.1016/S0079-6611(98)00016-0}, 1100 1097 year = {1998}, … … 1106 1103 loceanbibid = {01846}, 1107 1104 timestamp={20121014}, 1108 title = {{Twelve monthly experiments of 4D-variational assimilation in the tropical Atlantic during 1987. Part 2: Oceanographic interpretation}},1109 author = { E. Greiner and Sabine Arnault and A. Morlière},1110 language = { Anglais},1111 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1105 title = {{Twelve monthly experiments of 4D-variational assimilation in the tropical {A}tlantic during 1987. {P}art 2: {O}ceanographic interpretation}}, 1106 author = {{E}. {G}reiner and {S}abine {A}rnault and A. {M}orlière}, 1107 language = {{A}nglais}, 1108 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1112 1109 pages = {203-247}, 1113 journal = { Prog. Oceanogr.},1110 journal = {{P}rog. {O}ceanogr.}, 1114 1111 volume = {41}, 1115 1112 number = {2}, 1116 audience = {non sp {\'e}cifi{\'e}e},1113 audience = {non spécifiée}, 1117 1114 doi = {10.1016/S0079-6611(98)00017-2}, 1118 1115 year = {1998}, … … 1124 1121 loceanbibid = {01845}, 1125 1122 timestamp={20121014}, 1126 title = {{Low-frequency variability of the tropical Atlantic surface topography: altimetry and model comparison,}},1127 author = { Sabine Arnault and A. Morlière and J. Merle and Y. Ménard},1128 language = { Anglais},1129 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1123 title = {{Low-frequency variability of the tropical {A}tlantic surface topography: altimetry and model comparison,}}, 1124 author = {{S}abine {A}rnault and A. {M}orlière and J. {M}erle and Y. {M}énard}, 1125 language = {{A}nglais}, 1126 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1130 1127 pages = {14259-14288}, 1131 journal = { Journal of Geophysical Research},1128 journal = {{J}ournal of {G}eophysical {R}esearch}, 1132 1129 volume = {97}, 1133 1130 number = {C9}, 1134 audience = {non sp {\'e}cifi{\'e}e},1131 audience = {non spécifiée}, 1135 1132 doi = {10.1029/92JC00818}, 1136 1133 year = {1992}, … … 1142 1139 loceanbibid = {01844}, 1143 1140 timestamp={20121014}, 1144 title = {{Projection of future climate change conditions using IPCC simulations, neural networks and Bayesian statistics. Part 1: Temperature mean state and seasonal cycle in South America}},1145 author = { Jean-Philippe Boulanger and F. Martinez and E. C. Segura},1146 language = { Anglais},1147 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1141 title = {{Projection of future climate change conditions using IPCC simulations, neural networks and {B}ayesian statistics. {P}art 1: {T}emperature mean state and seasonal cycle in {S}outh {A}merica}}, 1142 author = {{J}ean-{P}hilippe {B}oulanger and F. {M}artinez and E. C. {S}egura}, 1143 language = {{A}nglais}, 1144 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1148 1145 pages = {233-259}, 1149 journal = { Climate Dynamics},1146 journal = {{C}limate {D}ynamics}, 1150 1147 volume = {27}, 1151 1148 number = {2-3}, 1152 audience = {non sp {\'e}cifi{\'e}e},1149 audience = {non spécifiée}, 1153 1150 doi = {10.1007/s00382-006-0134-8}, 1154 1151 year = {2006}, … … 1160 1157 loceanbibid = {01843}, 1161 1158 timestamp={20121014}, 1162 title = {{Projection of future climate change conditions using IPCC simulations, neural networks and Bayesian statistics. Part 2: Precipitation mean state and seasonal cycle in South America}},1163 author = { Jean-Philippe Boulanger and F. Martinez and E. C. Segura},1164 language = { Anglais},1165 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1159 title = {{Projection of future climate change conditions using IPCC simulations, neural networks and {B}ayesian statistics. {P}art 2: {P}recipitation mean state and seasonal cycle in {S}outh {A}merica}}, 1160 author = {{J}ean-{P}hilippe {B}oulanger and F. {M}artinez and E. C. {S}egura}, 1161 language = {{A}nglais}, 1162 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1166 1163 pages = {255-271}, 1167 journal = { Climate Dynamics},1164 journal = {{C}limate {D}ynamics}, 1168 1165 volume = {28}, 1169 1166 number = {2-3}, 1170 audience = {non sp {\'e}cifi{\'e}e},1167 audience = {non spécifiée}, 1171 1168 doi = {10.1007/s00382-006-0182-0}, 1172 1169 year = {2006}, … … 1178 1175 loceanbibid = {01842}, 1179 1176 timestamp={20121014}, 1180 title = {{Long Equatorial Waves in a High-Resolution OGCM Simulation of the Tropical Pacific Ocean during the 1985-94 TOGA Period}},1181 author = { Jean-Philippe Boulanger and Pascale Delecluse and C. Maes and Claire Lévy},1182 language = { Anglais},1183 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1177 title = {{Long {E}quatorial {W}aves in a {H}igh-{R}esolution OGCM {S}imulation of the {T}ropical {P}acific {O}cean during the 1985-94 TOGA {P}eriod}}, 1178 author = {{J}ean-{P}hilippe {B}oulanger and {P}ascale {D}elecluse and C. {M}aes and {C}laire {L}évy}, 1179 language = {{A}nglais}, 1180 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1184 1181 pages = {972-984}, 1185 journal = { Mon. Wea. Rev.},1182 journal = {{M}on. {W}ea. {R}ev.}, 1186 1183 volume = {125}, 1187 1184 number = {5}, 1188 audience = {non sp {\'e}cifi{\'e}e},1185 audience = {non spécifiée}, 1189 1186 doi = {10.1175/1520-0493(1997)1252.0.CO;2}, 1190 1187 year = {1997}, … … 1196 1193 loceanbibid = {01841}, 1197 1194 timestamp={20121014}, 1198 title = {{Yucatan Channel flow: Observations versus CLIPPER ATL6 and MERCATOR PAM models}},1199 author = { J. Candela and S. Tanahara and Michel Crépon and B. Barnier and J. Sheinbaum},1200 language = { Anglais},1201 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1195 title = {{Yucatan {C}hannel flow: {O}bservations versus CLIPPER ATL6 and MERCATOR PAM models}}, 1196 author = {{J}. {C}andela and S. {T}anahara and {M}ichel {C}répon and B. {B}arnier and J. {S}heinbaum}, 1197 language = {{A}nglais}, 1198 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1202 1199 pages = {3385}, 1203 journal = { Journal of Geophysical Research},1200 journal = {{J}ournal of {G}eophysical {R}esearch}, 1204 1201 volume = {108}, 1205 1202 number = {C12}, 1206 audience = {non sp {\'e}cifi{\'e}e},1203 audience = {non spécifiée}, 1207 1204 doi = {10.1029/2003JC001961}, 1208 1205 year = {2003}, … … 1214 1211 loceanbibid = {01840}, 1215 1212 timestamp={20121014}, 1216 title = {{A three-dimensional numerical study of deep water formation in the Northwestern Mediterranean Sea}},1217 author = { Gurvan Madec and M. Chartier and Pascale Delécluse and Michel Cr{\'e}pon},1218 language = { Anglais},1219 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1213 title = {{A three-dimensional numerical study of deep water formation in the {N}orthwestern {M}editerranean {S}ea}}, 1214 author = {{G}urvan {M}adec and M. {C}hartier and {P}ascale {D}elécluse and {M}ichel {C}répon}, 1215 language = {{A}nglais}, 1216 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1220 1217 pages = {1349-1371}, 1221 journal = { J. Phys. Oceanogr.},1218 journal = {{J}. {P}hys. {O}ceanogr.}, 1222 1219 volume = {21}, 1223 1220 number = {9}, 1224 audience = {non sp {\'e}cifi{\'e}e},1221 audience = {non spécifiée}, 1225 1222 doi = {10.1175/1520-0485(1991)0212.0.CO;2}, 1226 1223 year = {1991}, … … 1232 1229 loceanbibid = {01839}, 1233 1230 timestamp={20121014}, 1234 title = {{An intercomparison between four tropical ocean models : Thermocline variability}},1235 author = { Claude Frankignoul Sylvie Février and Nathalie Sennéchael and K. Verbeek and Pascale Braconnot},1236 language = { Anglais},1237 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1231 title = {{An intercomparison between four tropical ocean models : {T}hermocline variability}}, 1232 author = {{C}laude {F}rankignoul and {S}ylvie {F}évrier and {N}athalie {S}ennéchael and K. {V}erbeek and {P}ascale {B}raconnot}, 1233 language = {{A}nglais}, 1234 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1238 1235 pages = {351-364}, 1239 journal = { Tellus Series A : Dynamic meteorology and oceanography},1236 journal = {{T}ellus {S}eries A : {D}ynamic meteorology and oceanography}, 1240 1237 volume = {47}, 1241 1238 number = {3}, 1242 audience = {non sp {\'e}cifi{\'e}e},1239 audience = {non spécifiée}, 1243 1240 doi = {10.1034/j.1600-0870.1995.t01-2-00005.x}, 1244 1241 year = {1995}, … … 1250 1247 loceanbibid = {01838}, 1251 1248 timestamp={20121014}, 1252 title = {{On the ability of the LODYC GCM to simulate the thermocline depth in the equatorial Atlantic}},1253 author = { Pascale Braconnot and Claude Frankignoul},1254 language = { Anglais},1255 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1249 title = {{On the ability of the LODYC GCM to simulate the thermocline depth in the equatorial {A}tlantic}}, 1250 author = {{P}ascale {B}raconnot and {C}laude {F}rankignoul}, 1251 language = {{A}nglais}, 1252 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1256 1253 pages = {221-234}, 1257 journal = { Climate Dynamics},1254 journal = {{C}limate {D}ynamics}, 1258 1255 volume = {9}, 1259 1256 number = {4-5}, 1260 audience = {non sp {\'e}cifi{\'e}e},1257 audience = {non spécifiée}, 1261 1258 doi = {10.1007/s003820050021}, 1262 1259 year = {1994}, … … 1268 1265 loceanbibid = {01837}, 1269 1266 timestamp={20121014}, 1270 title = {{Testing, Model Simulations of the Thermocline Depth Variability in the Tropical Atlantic from 1982 through 1984}},1271 author = { Pascale Braconnot and Claude Frankignoul},1272 language = { Anglais},1273 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1267 title = {{Testing, {M}odel {S}imulations of the {T}hermocline {D}epth {V}ariability in the {T}ropical {A}tlantic from 1982 through 1984}}, 1268 author = {{P}ascale {B}raconnot and {C}laude {F}rankignoul}, 1269 language = {{A}nglais}, 1270 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1274 1271 pages = {626-647}, 1275 journal = { J. Phys. Oceanogr.},1272 journal = {{J}. {P}hys. {O}ceanogr.}, 1276 1273 volume = {23}, 1277 1274 number = {4}, 1278 audience = {non sp {\'e}cifi{\'e}e},1275 audience = {non spécifiée}, 1279 1276 doi = {10.1175/1520-0485(1993)0232.0.CO;2}, 1280 1277 year = {1993}, … … 1286 1283 loceanbibid = {01836}, 1287 1284 timestamp={20121014}, 1288 title = {{Distributed Ocean-Atmosphere Modeling and Sensitivity to the Coupling Flux Precision: The CATHODe Project}},1289 author = { C. Cassou and P. Noyret and E. Sevault and O. Thual and L. Terray and D. Beaucourt and M. Imbard},1290 language = { Anglais},1291 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1285 title = {{Distributed {O}cean-{A}tmosphere {M}odeling and {S}ensitivity to the {C}oupling {F}lux {P}recision: {T}he CATHODe {P}roject}}, 1286 author = {{C}. {C}assou and P. {N}oyret and E. {S}evault and O. {T}hual and L. {T}erray and D. {B}eaucourt and M. {I}mbard}, 1287 language = {{A}nglais}, 1288 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1292 1289 pages = {1035-1053}, 1293 journal = { Mon. Wea. Rev.},1290 journal = {{M}on. {W}ea. {R}ev.}, 1294 1291 volume = {126}, 1295 1292 number = {4}, 1296 audience = {non sp {\'e}cifi{\'e}e},1293 audience = {non spécifiée}, 1297 1294 doi = {10.1175/1520-0493(1998)1262.0.CO;2}, 1298 1295 year = {1998}, … … 1303 1300 loceanbibid = {01835}, 1304 1301 timestamp={20121014}, 1305 title = {{OPA 8.1 Ocean General Circulation Model reference manual}},1306 author = { Gurvan Madec and Pascale Delécluse and M. Imbard and Claire Lévy},1307 language = { Anglais},1308 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1302 title = {{OPA 8.1 {O}cean {G}eneral {C}irculation {M}odel reference manual}}, 1303 author = {{G}urvan {M}adec and {P}ascale {D}elécluse and M. {I}mbard and {C}laire {L}évy}, 1304 language = {{A}nglais}, 1305 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1309 1306 pages = {91p}, 1310 journal = { Note du Pole de Mod{\'e}lisation, Institut Pierre-Simon Laplace},1307 journal = {{N}ote du {P}ole de {M}odélisation, {I}nstitut {P}ierre-{S}imon {L}aplace}, 1311 1308 volume = {11}, 1312 audience = {non sp {\'e}cifi{\'e}e},1309 audience = {non spécifiée}, 1313 1310 year = {1998}, 1314 1311 comment = {20121114 : ++ compléter prénom dans hal}, … … 1319 1316 loceanbibid = {01834}, 1320 1317 timestamp={20121014}, 1321 title = {{Simulation of the nitrate seasonal cycle in the equatorial Atlantic Ocean during 1983 and 1984}},1322 author = { H. Loukos and Laurent Mémery},1323 language = { Anglais},1324 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1318 title = {{Simulation of the nitrate seasonal cycle in the equatorial {A}tlantic {O}cean during 1983 and 1984}}, 1319 author = {{H}. {L}oukos and {L}aurent {M}émery}, 1320 language = {{A}nglais}, 1321 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1325 1322 pages = {15549-15573}, 1326 journal = { Journal of Geophysical Research},1323 journal = {{J}ournal of {G}eophysical {R}esearch}, 1327 1324 volume = {104}, 1328 1325 number = {C7}, 1329 audience = {non sp {\'e}cifi{\'e}e},1326 audience = {non spécifiée}, 1330 1327 doi = {10.1029/1999JC900084}, 1331 1328 year = {1999}, … … 1336 1333 loceanbibid = {01833}, 1337 1334 timestamp={20121014}, 1338 title = {{Sensibility study of an Oceanic General Circulation Model forced by satellite wind-stress fields}},1339 author = { N. Grima and A. Bentamy and K. Katsaros and Y. Quilfen and P. Delecluse and C. Lévy},1340 language = { Anglais},1341 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1335 title = {{Sensibility study of an {O}ceanic {G}eneral {C}irculation {M}odel forced by satellite wind-stress fields}}, 1336 author = {{N}. {G}rima and A. {B}entamy and K. {K}atsaros and Y. {Q}uilfen and P. {D}elecluse and C. {L}évy}, 1337 language = {{A}nglais}, 1338 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1342 1339 pages = {7967-7989}, 1343 journal = { Journal of Geophysical Research},1340 journal = {{J}ournal of {G}eophysical {R}esearch}, 1344 1341 volume = {104}, 1345 1342 number = {C4}, 1346 audience = {non sp {\'e}cifi{\'e}e},1343 audience = {non spécifiée}, 1347 1344 doi = {10.1029/1999JC900007}, 1348 1345 year = {1999}, … … 1355 1352 timestamp={20121014}, 1356 1353 title = {{Climatology and interannual variability simulated by the ARPEGE-OPA coupled model}}, 1357 author = { L. Terray and O. Thual and S. Belamari and M. Déqué and P. Din and P. Delecluse and C. Lévy},1358 language = { Anglais},1359 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1354 author = {{L}. {T}erray and O. {T}hual and S. {B}elamari and M. {D}équé and P. {D}in and P. {D}elecluse and C. {L}évy}, 1355 language = {{A}nglais}, 1356 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1360 1357 pages = {487-505}, 1361 journal = { Climate Dynamics},1358 journal = {{C}limate {D}ynamics}, 1362 1359 volume = {11}, 1363 1360 number = {8}, 1364 audience = {non sp {\'e}cifi{\'e}e},1361 audience = {non spécifiée}, 1365 1362 doi = {10.1007/BF00207197}, 1366 1363 year = {1995}, … … 1373 1370 timestamp={20121014}, 1374 1371 title = {{Will marine dimethylsulfide emissions amplify or alleviate global warming? A model study}}, 1375 author = { Laurent Bopp and O. Boucher and Olivier Aumont and S. Belviso and J.-L. Dufresneand M. Pham and P. Monfray},1376 language = { Anglais},1377 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Service d'a{\'e}ronomie - SA},1372 author = {{L}aurent {B}opp and O. {B}oucher and {O}livier {A}umont and S. {B}elviso and Jean-Louis {D}ufresne and M. {P}ham and P. {M}onfray}, 1373 language = {{A}nglais}, 1374 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {S}ervice d'aéronomie - SA}, 1378 1375 pages = {826-835}, 1379 journal = { Canadian Journal of Fisheries and Aquatic Sciences},1376 journal = {{C}anadian {J}ournal of {F}isheries and {A}quatic {S}ciences}, 1380 1377 volume = {61}, 1381 1378 number = {5}, 1382 audience = {non sp {\'e}cifi{\'e}e},1379 audience = {non spécifiée}, 1383 1380 doi = {10.1139/F04-045}, 1384 1381 year = {2004}, … … 1390 1387 timestamp={20121014}, 1391 1388 title = {{Sensitivity study of dimethylsulphide (DMS) atmospheric concentrations and sulphate aerosol indirect radiative forcing to the DMS source representation and oxidation}}, 1392 author = { O. Boucher and C. Moulin and S. Belviso and Olivier Aumont and Laurent Bopp and E. Cosme and R. Von Kuhlmann and M. G. Lawrence and M. Pham and M. S. Reddy and J. Sciare and C. Venkataraman},1393 language = { Anglais},1394 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Service d'a{\'e}ronomie - SA},1389 author = {{O}. {B}oucher and C. {M}oulin and S. {B}elviso and {O}livier {A}umont and {L}aurent {B}opp and E. {C}osme and R. {V}on {K}uhlmann and M. G. {L}awrence and M. {P}ham and M. S. {R}eddy and J. {S}ciare and C. {V}enkataraman}, 1390 language = {{A}nglais}, 1391 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {S}ervice d'aéronomie - SA}, 1395 1392 pages = {1181-1216}, 1396 journal = { Atmospheric Chemistry and Physics Discussions},1393 journal = {{A}tmospheric {C}hemistry and {P}hysics {D}iscussions}, 1397 1394 volume = {2}, 1398 audience = {non sp {\'e}cifi{\'e}e},1395 audience = {non spécifiée}, 1399 1396 year = {2002}, 1400 1397 comment = {20121114 : doublon hal-00203649}, … … 1407 1404 title = {{Correction to "A global diagnostic of interior ocean ventilation"}}, 1408 1405 author = {{B}runo {B}lanke and {S}abrina {S}peich and {G}urvan {M}adec and {R}. {M}augé}, 1409 language = { Anglais},1410 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1406 language = {{A}nglais}, 1407 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1411 1408 pages = {1625}, 1412 journal = { Geophysical Research Letters},1409 journal = {{G}eophysical {R}esearch {L}etters}, 1413 1410 volume = {29}, 1414 1411 number = {13}, 1415 audience = {non sp {\'e}cifi{\'e}e},1412 audience = {non spécifiée}, 1416 1413 doi = {10.1029/2002GL015635}, 1417 1414 year = {2002}, … … 1423 1420 loceanbibid = {01829}, 1424 1421 timestamp={20121014}, 1425 title = {{Observed precipitation in the Paran{\'a}-Plata hydrological basin: long-term trends, extreme conditions and ENSO teleconnections}},1426 author = { J.-P. Boulanger and J. Leloup and O. Panalba and M. Rusticucci and F. Lafon and W. Vargas},1427 language = { Anglais},1428 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1422 title = {{Observed precipitation in the {P}araná-{P}lata hydrological basin: long-term trends, extreme conditions and ENSO teleconnections}}, 1423 author = {{J}ean-{P}hilippe {B}oulanger and Julie {L}eloup and O. {P}analba and M. {R}usticucci and F. {L}afon and W. {V}argas}, 1424 language = {{A}nglais}, 1425 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1429 1426 pages = {393-413}, 1430 journal = { Climate Dynamics},1427 journal = {{C}limate {D}ynamics}, 1431 1428 volume = {24}, 1432 1429 number = {4}, 1433 audience = {non sp {\'e}cifi{\'e}e},1430 audience = {non spécifiée}, 1434 1431 doi = {10.1007/s00382-004-0514-x}, 1435 1432 year = {2005}, … … 1442 1439 timestamp={20121014}, 1443 1440 title = {{Analysis of a potential "solar radiation dose--dimethylsulfide--cloud condensation nuclei" link from globally mapped seasonal correlations}}, 1444 author = { S. M. Vallina and R. Simó and S. Gassó and Clément De Boyer-Montégut and E. Del Río and E. Jurado and J. Dachs},1445 language = { Anglais},1446 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1441 author = {{S}. M. {V}allina and R. {S}imó and S. {G}assó and {C}lément {D}e {B}oyer-{M}ontégut and E. {D}el {R}ío and E. {J}urado and J. {D}achs}, 1442 language = {{A}nglais}, 1443 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1447 1444 pages = {GB2004}, 1448 journal = { Global Biogeochem. Cycles},1445 journal = {{G}lobal {B}iogeochem. {C}ycles}, 1449 1446 volume = {21}, 1450 audience = {non sp {\'e}cifi{\'e}e},1447 audience = {non spécifiée}, 1451 1448 doi = {10.1029/2006GB002787}, 1452 1449 year = {2007}, … … 1459 1456 timestamp={20121014}, 1460 1457 title = {{Du temps qui passe au temps qu'il fera}}, 1461 author = { Maxence Revault D'Allonnes},1462 language = { Fran{\c c}ais},1463 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1458 author = {{M}axence {R}evault D'{A}llonnes}, 1459 language = {{F}rançais}, 1460 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1464 1461 pages = {25-26}, 1465 1462 journal = {GEOCHRONIQUES}, 1466 1463 volume = {98}, 1467 audience = {non sp {\'e}cifi{\'e}e},1464 audience = {non spécifiée}, 1468 1465 year = {2006}, 1469 1466 comment = {20121114 : ++ compléter prénom dans hal}, … … 1474 1471 loceanbibid = {01827}, 1475 1472 timestamp={20121014}, 1476 title = {{Effects of climate and different management strategies on Aedes aegypti breeding sites: a longitudinal survey in Brasilia (DF, Brazil)}},1477 author = { Charly Favier and Nicolas Dégallier and Paulo De Tarso Ribeiro Vilarinhos and Maria Do Socorro Laurentino De Carvalho and Maria Amelia Cavalcanti Yoshizawa and Monique Britto Knox},1478 language = { Anglais},1479 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1473 title = {{Effects of climate and different management strategies on {A}edes aegypti breeding sites: a longitudinal survey in {B}rasilia (DF, {B}razil)}}, 1474 author = {{C}harly {F}avier and {N}icolas {D}égallier and {P}aulo {D}e {T}arso {R}ibeiro {V}ilarinhos and {M}aria {D}o {S}ocorro {L}aurentino {D}e {C}arvalho and {M}aria {A}melia {C}avalcanti {Y}oshizawa and {M}onique {B}ritto {K}nox}, 1475 language = {{A}nglais}, 1476 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1480 1477 pages = {1104-1118}, 1481 journal = { Tropical Medicine \& International Health},1478 journal = {{T}ropical {M}edicine \& {I}nternational {H}ealth}, 1482 1479 volume = {11}, 1483 1480 number = {7}, 1484 audience = {non sp {\'e}cifi{\'e}e},1481 audience = {non spécifiée}, 1485 1482 doi = {10.1111/j.1365-3156.2006.01653.x}, 1486 1483 year = {2006}, … … 1492 1489 loceanbibid = {01826}, 1493 1490 timestamp={20121014}, 1494 title = {{Susceptibility of Aedes aegypti larvae to the insecticide temephos in the Federal District, Brazil}},1495 author = { Maria Do Socorro Laurentino De Carvalho and Eloísa Dutra Caldas and Nicolas Dégallier and Paulo De Tarso Ribeiro Vilarinhos and Luís César Kenupp Rodrigues De Souza and Maria Amélia Cavalcanti Yoshizawa and Monique Britto Knox and Cristiane De Oliveira},1496 language = { Anglais},1497 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1491 title = {{Susceptibility of {A}edes aegypti larvae to the insecticide temephos in the {F}ederal {D}istrict, {B}razil}}, 1492 author = {{M}aria {D}o {S}ocorro {L}aurentino {D}e {C}arvalho and {E}loísa {D}utra {C}aldas and {N}icolas {D}égallier and {P}aulo {D}e {T}arso {R}ibeiro {V}ilarinhos and {L}uís {C}ésar {K}enupp {R}odrigues {D}e {S}ouza and {M}aria {A}mélia {C}avalcanti {Y}oshizawa and {M}onique {B}ritto {K}nox and {C}ristiane {D}e {O}liveira}, 1493 language = {{A}nglais}, 1494 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1498 1495 pages = {623-629}, 1499 journal = { Rev. Sa{\'u}de p{\'u}b.},1496 journal = {{R}ev. {S}aúde púb.}, 1500 1497 volume = {38}, 1501 1498 number = {5}, 1502 1499 note = {http://www.scielo.br/scielo.php?script=sci\_arttext\&pid=S0034-89102004000500002\&lng=en\&nrm=iso}, 1503 audience = {non sp {\'e}cifi{\'e}e},1500 audience = {non spécifiée}, 1504 1501 year = {2004}, 1505 1502 } … … 1509 1506 loceanbibid = {01825}, 1510 1507 timestamp={20121014}, 1511 title = {{Etude par pi {\`e}geage lumineux de l'abondance saisonni{\`e}re d'insectes forestiers en Guyane fran{\c c}aise}},1512 author = { Nicolas Dégallier and P. Charles-Dominique and H. Gérard},1513 language = { Fran{\c c}ais},1514 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1508 title = {{Etude par piègeage lumineux de l'abondance saisonnière d'insectes forestiers en {G}uyane française}}, 1509 author = {{N}icolas {D}égallier and P. {C}harles-{D}ominique and H. {G}érard}, 1510 language = {{F}rançais}, 1511 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1515 1512 pages = {473-484}, 1516 journal = { Bull. Soc. ent. Fr.},1513 journal = {{B}ull. {S}oc. ent. {F}r.}, 1517 1514 volume = {109}, 1518 1515 number = {5}, 1519 audience = {non sp {\'e}cifi{\'e}e},1516 audience = {non spécifiée}, 1520 1517 year = {2004}, 1521 1518 comment = {20121114 : ++ compléter diacritique dans nom dans hal}, … … 1526 1523 loceanbibid = {01824}, 1527 1524 timestamp={20121014}, 1528 title = {{Larvicidal activity of some Cerrado plant extracts against Aedes aegypti}},1529 author = { A. M. S. Rodrigues and J. E. De Paula and Nicolas Degallier and Jean-François Molez and L. S. Espindola},1530 language = { Anglais},1531 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1525 title = {{Larvicidal activity of some {C}errado plant extracts against {A}edes aegypti}}, 1526 author = {{A}. M. S. {R}odrigues and J. E. {D}e {P}aula and {N}icolas {D}égallier and {J}ean-{F}rançois {M}olez and L. S. {E}spindola}, 1527 language = {{A}nglais}, 1528 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1532 1529 pages = {314-317}, 1533 journal = { Journal of the American Mosquito Control Association, 2006, 22 (2), p. 314-317.},1530 journal = {{J}ournal of the {A}merican {M}osquito {C}ontrol {A}ssociation, 2006, 22 (2), p. 314-317.}, 1534 1531 volume = {22}, 1535 1532 number = {2}, 1536 audience = {non sp {\'e}cifi{\'e}e},1533 audience = {non spécifiée}, 1537 1534 doi = {10.2987/8756-971X(2006)22[314:LAOSCP]2.0.CO;2}, 1538 1535 year = {2006}, … … 1544 1541 loceanbibid = {01823}, 1545 1542 timestamp={20121014}, 1546 title = {{Apparition des premiers cas autochtones caus {\'e}s par le s{\'e}rotype Dengue-3 dans le District f{\'e}d{\'e}ral, Br{\'e}sil}},1547 author = {J.M.S. Teixeira and A.J.M. Chaib and H.P. Silva and J.L. Souza and Jean-François Molez and Nicolas Dégallier},1548 language = { Anglais},1549 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1543 title = {{Apparition des premiers cas autochtones causés par le sérotype {D}engue-3 dans le {D}istrict fédéral, {B}résil}}, 1544 author = {J.M.S. {T}eixeira and A.J.M. {C}haib and H.P. {S}ilva and J.L. {S}ouza and {J}ean-{F}rançois {M}olez and {N}icolas {D}égallier}, 1545 language = {{A}nglais}, 1546 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1550 1547 pages = {85-89}, 1551 journal = { Bulletin de la Soci{\'e}t{\'e} de Pathologie Exotique},1548 journal = {{B}ulletin de la {S}ociété de {P}athologie {E}xotique}, 1552 1549 volume = {99}, 1553 1550 number = {2}, 1554 audience = {non sp {\'e}cifi{\'e}e},1551 audience = {non spécifiée}, 1555 1552 year = {2006}, 1556 1553 } … … 1560 1557 loceanbibid = {01822}, 1561 1558 timestamp={20121014}, 1562 title = {{An indirect estimation of the developmental time of Haemagogus janthinomys (Diptera : Culicidae), the main vector of yellow fever in South America}},1563 author = { Nicolas Dégallier and H.A. De Oliveira Monteiro and F.C. Castro and O.V. Da Silva and G.C. Sa Filho and Eric Elguero},1564 language = { Anglais},1565 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1559 title = {{An indirect estimation of the developmental time of {H}aemagogus janthinomys (Diptera : {C}ulicidae), the main vector of yellow fever in {S}outh {A}merica}}, 1560 author = {{N}icolas {D}égallier and H.A. {D}e {O}liveira {M}onteiro and F.C. {C}astro and O.V. {D}a {S}ilva and G.C. {S}a {F}ilho and {E}ric {E}lguero}, 1561 language = {{A}nglais}, 1562 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1566 1563 pages = {117-122}, 1567 journal = { Studies on Neotropical Fauna and Environment},1564 journal = {{S}tudies on {N}eotropical {F}auna and {E}nvironment}, 1568 1565 volume = {41}, 1569 1566 number = {2}, 1570 audience = {non sp {\'e}cifi{\'e}e},1567 audience = {non spécifiée}, 1571 1568 doi = {10.1080/01650520500398662}, 1572 1569 year = {2006}, … … 1577 1574 loceanbibid = {01821}, 1578 1575 timestamp={20121014}, 1579 title = {{Scanning electron Microscopy study of the egg of Haemagogus (Haemagogus) capricornii Lutz, 1904 (Diptera : Culicidae)}},1580 author = { J. Alencar and A. E. Guimaraes and R. P. Mello and C. M. Lopes and Nicolas Dégallier and J. R. Santos Mallet},1581 language = { Anglais},1582 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1576 title = {{Scanning electron {M}icroscopy study of the egg of {H}aemagogus (Haemagogus) capricornii {L}utz, 1904 (Diptera : {C}ulicidae)}}, 1577 author = {{J}. {A}lencar and A. E. {G}uimaraes and R. P. {M}ello and C. M. {L}opes and {N}icolas {D}égallier and J. R. {S}antos {M}allet}, 1578 language = {{A}nglais}, 1579 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1583 1580 pages = {1-6}, 1584 journal = { Journal of Medical Entomology},1581 journal = {{J}ournal of {M}edical {E}ntomology}, 1585 1582 volume = {42}, 1586 1583 number = {1}, 1587 audience = {non sp {\'e}cifi{\'e}e},1584 audience = {non spécifiée}, 1588 1585 doi = {10.1603/0022-2585(2005)042[0001:SEMSOT]2.0.CO;2}, 1589 1586 year = {2005}, … … 1595 1592 loceanbibid = {01820}, 1596 1593 timestamp={20121014}, 1597 title = {{Plastysoma directum Lewis, 1885, esp{\`e}ce rescap{\'e}e de l'oubli (Coleoptera, Histeridae, Histerinae, Platysomatini)}},1598 author = { Nicolas Dégallier and Y. Gomy and M. Brendell},1599 language = { Anglais},1600 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1594 title = {{Plastysoma directum {L}ewis, 1885, espèce rescapée de l'oubli (Coleoptera, {H}isteridae, {H}isterinae, {P}latysomatini)}}, 1595 author = {{N}icolas {D}égallier and Y. {G}omy and M. {B}rendell}, 1596 language = {{A}nglais}, 1597 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1601 1598 pages = {180-182}, 1602 journal = { Nouvelle Revue d'Entomologie},1599 journal = {{N}ouvelle {R}evue d'{E}ntomologie}, 1603 1600 volume = {22}, 1604 1601 number = {2}, 1605 audience = {non sp {\'e}cifi{\'e}e},1602 audience = {non spécifiée}, 1606 1603 year = {2005}, 1607 1604 } … … 1611 1608 loceanbibid = {01819}, 1612 1609 timestamp={20121014}, 1613 title = {{Notes taxonomiques sur les Chlamydopsinae et descriptions d'esp{\`e}ces nouvelles : 1. Genres Ceratohister Reichensperger, Eucurtiopsis Silvestri et Orectoscelis Lewis (Coleoptera, Histeridae)}},1614 author = { Nicolas D{\'e}gallier and M.S. Casterino},1615 language = { Anglais},1616 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1610 title = {{Notes taxonomiques sur les {C}hlamydopsinae et descriptions d'espèces nouvelles : 1. {G}enres {C}eratohister {R}eichensperger, {E}ucurtiopsis {S}ilvestri et {O}rectoscelis {L}ewis (Coleoptera, {H}isteridae)}}, 1611 author = {{N}icolas {D}égallier and M.S. {C}asterino}, 1612 language = {{A}nglais}, 1613 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1617 1614 pages = {299-326}, 1618 journal = { Bulletin de la Soci{\'e}t{\'e} Entomologique de France},1615 journal = {{B}ulletin de la {S}ociété {E}ntomologique de {F}rance}, 1619 1616 volume = {110}, 1620 1617 number = {3}, 1621 audience = {non sp {\'e}cifi{\'e}e},1618 audience = {non spécifiée}, 1622 1619 year = {2005}, 1623 1620 } … … 1627 1624 loceanbibid = {01818}, 1628 1625 timestamp={20121014}, 1629 title = {{Notes taxonomiques sur les Chlamydopsinae et descriptions d'esp{\`e}ces nouvelles : 2. Genre Pheidoliphila Lea (Coleoptera, Histeridae)}},1630 author = { Nicolas D{\'e}gallier and M.S. Casterino},1631 language = { Anglais},1632 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1626 title = {{Notes taxonomiques sur les {C}hlamydopsinae et descriptions d'espèces nouvelles : 2. {G}enre {P}heidoliphila {L}ea (Coleoptera, {H}isteridae)}}, 1627 author = {{N}icolas {D}égallier and M.S. {C}asterino}, 1628 language = {{A}nglais}, 1629 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1633 1630 pages = {463-494}, 1634 journal = { Bulletin de la Soci{\'e}t{\'e} Entomologique de France},1631 journal = {{B}ulletin de la {S}ociété {E}ntomologique de {F}rance}, 1635 1632 volume = {110}, 1636 1633 number = {4-5}, 1637 audience = {non sp {\'e}cifi{\'e}e},1634 audience = {non spécifiée}, 1638 1635 year = {2005}, 1639 1636 } … … 1643 1640 loceanbibid = {01817}, 1644 1641 timestamp={20121014}, 1645 title = {{Coleoptera histeridae de Guyane fran{\c c}aise : 4. Myrm{\'e}cophiles et termitophiles de la sous-famille des hetaeriinae : notes techniques, faunistiques et taxonomiques}},1646 author = { Nicolas D{\'e}gallier},1647 language = { Anglais},1648 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1642 title = {{Coleoptera histeridae de {G}uyane française : 4. {M}yrmécophiles et termitophiles de la sous-famille des hetaeriinae : notes techniques, faunistiques et taxonomiques}}, 1643 author = {{N}icolas {D}égallier}, 1644 language = {{A}nglais}, 1645 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1649 1646 pages = {293-316}, 1650 journal = { Bulletin de la Soci{\'e}t{\'e} Entomologique de France},1647 journal = {{B}ulletin de la {S}ociété {E}ntomologique de {F}rance}, 1651 1648 volume = {109}, 1652 1649 number = {3}, 1653 audience = {non sp {\'e}cifi{\'e}e},1650 audience = {non spécifiée}, 1654 1651 year = {2004}, 1655 1652 } … … 1659 1656 loceanbibid = {01816}, 1660 1657 timestamp={20121014}, 1661 title = {{Wind speed effect on L-band brightness temperature inferred from EuroSTARRS and WISE 2001 field experiments}},1662 author = { J. Etcheto and E. Dinnat and Jacquelin Boutin and A. Camps and J. Miller and S. Contardo and J. Wesson and J. Font and D. Long},1663 language = { Anglais},1664 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1658 title = {{Wind speed effect on L-band brightness temperature inferred from {E}uroSTARRS and WISE 2001 field experiments}}, 1659 author = {{J}. {E}tcheto and E. {D}innat and {J}acquelin {B}outin and A. {C}amps and J. {M}iller and S. {C}ontardo and J. {W}esson and J. {F}ont and D. {L}ong}, 1660 language = {{A}nglais}, 1661 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1665 1662 pages = {2206-2214}, 1666 journal = {IEEE Transactions on Geoscience and Remote Sensing},1663 journal = {IEEE {T}ransactions on {G}eoscience and {R}emote {S}ensing}, 1667 1664 volume = {42}, 1668 audience = {non sp {\'e}cifi{\'e}e},1665 audience = {non spécifiée}, 1669 1666 doi = {10.1109/TGRS.2004.834644}, 1670 1667 year = {2004}, … … 1677 1674 timestamp={20121014}, 1678 1675 title = {{Wavelet ridge diagnosis of time-varying elliptical signals with application to an oceanic eddy}}, 1679 author = { J. M. Lilly and Jean-Claude Gascard},1680 abstract = {{A method for diagnosing the physical properties of a time-varying ellipse is presented. This essentially involves extending the notion of instantaneous frequency to the bivariate case. New complications, and possibilities, arise from the fact that there are several meaningful forms in which a time-varying ellipse may be represented. A perturbation analysis valid for the near-circular case clarifies these issues. Diagnosis of the ellipse properties may then be performed using wavelet ridge analysis, and slowly-varying changes in the ellipse structure may be decoupled from the fast orbital motion through the use of elliptic integrals, without the need for additional explicit filtering. The theory is presented in parallel with an application to a position time series of a drifting subsurface float trapped in an oceanic eddy.}},1681 language = { Anglais},1682 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1676 author = {{J}. M. {L}illy and {J}ean-{C}laude {G}ascard}, 1677 abstract = {{A method for diagnosing the physical properties of a time-varying ellipse is presented. {T}his essentially involves extending the notion of instantaneous frequency to the bivariate case. {N}ew complications, and possibilities, arise from the fact that there are several meaningful forms in which a time-varying ellipse may be represented. A perturbation analysis valid for the near-circular case clarifies these issues. {D}iagnosis of the ellipse properties may then be performed using wavelet ridge analysis, and slowly-varying changes in the ellipse structure may be decoupled from the fast orbital motion through the use of elliptic integrals, without the need for additional explicit filtering. {T}he theory is presented in parallel with an application to a position time series of a drifting subsurface float trapped in an oceanic eddy.}}, 1678 language = {{A}nglais}, 1679 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1683 1680 pages = {467-483}, 1684 journal = { Nonlinear Processes in Geophysics},1681 journal = {{N}onlinear {P}rocesses in {G}eophysics}, 1685 1682 volume = {13}, 1686 1683 number = {5}, 1687 1684 note = {http://www.nonlin-processes-geophys.net/13/467/2006/}, 1688 audience = {non sp {\'e}cifi{\'e}e},1685 audience = {non spécifiée}, 1689 1686 year = {2006}, 1690 1687 comment = {20121114 : ++ compléter prénom dans hal}, … … 1695 1692 loceanbibid = {01814}, 1696 1693 timestamp={20121014}, 1697 title = {{On the deep water circulation of the eastern South Atlantic Ocean}},1698 author = { M. Arhan and H. Mercier and Y.-H. Park},1699 language = { Anglais},1700 affiliation = { Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1694 title = {{On the deep water circulation of the eastern {S}outh {A}tlantic {O}cean}}, 1695 author = {{M}. {A}rhan and H. {M}ercier and {Y}oung-{H}yang {P}ark}, 1696 language = {{A}nglais}, 1697 affiliation = {{L}aboratoire de physique des océans - LPO , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1701 1698 pages = {889-916(28)}, 1702 journal = { Deep Sea Research Part I Oceanographic Research Papers},1699 journal = {{D}eep {S}ea {R}esearch {P}art I {O}ceanographic {R}esearch {P}apers}, 1703 1700 volume = {50}, 1704 1701 number = {7}, 1705 audience = {non sp {\'e}cifi{\'e}e},1702 audience = {non spécifiée}, 1706 1703 doi = {10.1016/S0967-0637(03)00072-4}, 1707 1704 year = {2003}, … … 1713 1710 loceanbibid = {01813}, 1714 1711 timestamp={20121014}, 1715 title = {{Re-evaluation of the systematics of two deep-sea species of Thalassometra (Echinomermata: Crinoidea) and its biogeographical implications}},1716 author = { M. Eléaume and N. Améziane and Y.-H. Park},1717 abstract = {{Biogeography of deep-sea comatulid crinoids is poorly understood owing partly to the lack of detailed taxonomic studies. Recent cruises off Peru dredged up two new, well-preserved specimens of Thalassometra bispinosa, a deep-sea comatulid species which was heretofore only known from the Southern Ocean. These new records enabled re-evaluation of intra-specific variation for both quantitative and qualitative morphological characters. We thus provide a new description of the species, including these new specimens, and discuss the affinities with closely related species. As a consequence, we re-evaluate the systematic position of material previously assigned to T. bispinosa dredged from the Campbell Plateau, Southern Ocean. Discrete morphological characters, measurements and SEM photographs justify reassignment of these specimens to Thalassometra villosa. This species, another poorly known deep-sea comatulid crinoid previously known only from the Aleutian Islands in the North Pacific, is also redescribed. The biogeography of these two deep-sea comatulid species is discussed and hypotheses of their geographical distribution are proposed.}},1718 language = { Anglais},1719 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1712 title = {{Re-evaluation of the systematics of two deep-sea species of {T}halassometra (Echinomermata: {C}rinoidea) and its biogeographical implications}}, 1713 author = {{M}. {E}léaume and N. {A}méziane and {Y}oung-{H}yang {P}ark}, 1714 abstract = {{Biogeography of deep-sea comatulid crinoids is poorly understood owing partly to the lack of detailed taxonomic studies. {R}ecent cruises off {P}eru dredged up two new, well-preserved specimens of {T}halassometra bispinosa, a deep-sea comatulid species which was heretofore only known from the {S}outhern {O}cean. {T}hese new records enabled re-evaluation of intra-specific variation for both quantitative and qualitative morphological characters. {W}e thus provide a new description of the species, including these new specimens, and discuss the affinities with closely related species. {A}s a consequence, we re-evaluate the systematic position of material previously assigned to T. bispinosa dredged from the {C}ampbell {P}lateau, {S}outhern {O}cean. {D}iscrete morphological characters, measurements and SEM photographs justify reassignment of these specimens to {T}halassometra villosa. {T}his species, another poorly known deep-sea comatulid crinoid previously known only from the {A}leutian {I}slands in the {N}orth {P}acific, is also redescribed. {T}he biogeography of these two deep-sea comatulid species is discussed and hypotheses of their geographical distribution are proposed.}}, 1715 language = {{A}nglais}, 1716 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1720 1717 pages = {1949-1968}, 1721 journal = { Journal of Natural History},1718 journal = {{J}ournal of {N}atural {H}istory}, 1722 1719 volume = {38}, 1723 1720 number = {15}, 1724 audience = {non sp {\'e}cifi{\'e}e},1721 audience = {non spécifiée}, 1725 1722 doi = {10.1080/0022290310001613566}, 1726 1723 year = {2004}, … … 1734 1731 loceanteam={varclim}, 1735 1732 loceanaffectation={cnrs,ird}, 1736 title = {{ {\'E}volution de notre compr{\'e}hension du syst{\`e}me de mousson ouest-africain}},1737 author = { Jean-Philippe Lafore and Nicole Asencio and Dominique Bouniol and Fleur Couvreux and Cyrille Flamant and Françoise Guichard and Nicholas Hall and Serge Janicot and Cécile Kocha and Christophe Lavaysse and Stéphanie Leroux and Emmanuel Poan and Philippe Peyrillé and Rémy Roca and Romain Roehrig and Frank Roux and Frédérique Saïd},1738 abstract = {{Since the pioneering GATE international field experiment in 1974, little progress had been made on the documentation and understanding of the West African Monsoon system. Ten years after the AMMA project was initiated, how has our knowledge of this monsoon evolved? Although the main actors of this atmosphere ocean-continent coupled system were already known, AMMA has allowed us to study thoroughly the details of the processes at play and their coupling. Starting from a static view of the system, a more dynamical view is now emerging, involving the whole Earth system : the whole African continent, mid-latitudes, the Indian monsoon and the entire tropical belt. This has opened new avenues of investigation into the intraseasonal variability of the West African monsoon.}},1739 keywords = { Mousson; Afrique; Dynamique; Jet; Couche limite de surface; Mod{\`e}le coupl{\'e} oc{\'e}an-atmosph{\`e}re; Ouest; Variabilit{\'e} temporelle; Saison; Campagne de mesure; Mod{\`e}le global; Zcit; Inde; Climat temp{\'e}r{\'e}; Humidit{\'e}; Vapeur d'eau; Thermocline},1740 language = { Fran{\c c}ais},1741 affiliation = { Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME , Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Universit{\'e} Paris 6, Pierre et Marie Curie - UPMC , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Department of Atmospheric and Oceanic Sciences, McGill University , Department of Atmospheric and Environmental Sciences , Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD , Laboratoire d'a{\'e}rologie - LA},1733 title = {{Évolution de notre compréhension du système de mousson ouest-africain}}, 1734 author = {{J}ean-{P}hilippe {L}afore and {N}icole {A}sencio and {D}ominique {B}ouniol and {F}leur {C}ouvreux and {C}yrille {F}lamant and {F}rançoise {G}uichard and {N}icholas {H}all and {S}erge {J}anicot and {C}écile {K}ocha and {C}hristophe {L}avaysse and {S}téphanie {L}eroux and {E}mmanuel {P}oan and {P}hilippe {P}eyrillé and {R}émy {R}oca and {R}omain {R}oehrig and {F}rank {R}oux and {F}rédérique {S}aïd}, 1735 abstract = {{Since the pioneering GATE international field experiment in 1974, little progress had been made on the documentation and understanding of the {W}est {A}frican {M}onsoon system. {T}en years after the AMMA project was initiated, how has our knowledge of this monsoon evolved? {A}lthough the main actors of this atmosphere ocean-continent coupled system were already known, AMMA has allowed us to study thoroughly the details of the processes at play and their coupling. {S}tarting from a static view of the system, a more dynamical view is now emerging, involving the whole {E}arth system : the whole {A}frican continent, mid-latitudes, the {I}ndian monsoon and the entire tropical belt. {T}his has opened new avenues of investigation into the intraseasonal variability of the {W}est {A}frican monsoon.}}, 1736 keywords = {{M}ousson; {A}frique; {D}ynamique; {J}et; {C}ouche limite de surface; {M}odèle couplé océan-atmosphère; {O}uest; {V}ariabilité temporelle; {S}aison; {C}ampagne de mesure; {M}odèle global; {Z}cit; {I}nde; {C}limat tempéré; {H}umidité; {V}apeur d'eau; {T}hermocline}, 1737 language = {{F}rançais}, 1738 affiliation = {{G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {U}niversité {P}aris 6, {P}ierre et {M}arie {C}urie - UPMC , {L}aboratoire d'études en {G}éophysique et océanographie spatiales - LEGOS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {D}epartment of {A}tmospheric and {O}ceanic {S}ciences, {M}cGill {U}niversity , {D}epartment of {A}tmospheric and {E}nvironmental {S}ciences , {L}aboratoire de {M}étéorologie {D}ynamique - LMD , {L}aboratoire d'aérologie - LA}, 1742 1739 pages = {11-16}, 1743 journal = { La M{\'e}t{\'e}orologie},1744 number = { Octobre, Sp{\'e}cial AMMA},1740 journal = {{L}a {M}étéorologie}, 1741 number = {{O}ctobre, {S}pécial AMMA}, 1745 1742 audience = {internationale}, 1746 1743 doi = {10.4267/2042/48127}, … … 1754 1751 loceanteam={varclim}, 1755 1752 loceanaffectation={cnrs,ird}, 1756 title = {{Les avanc {\'e}es d'AMMA sur les interactions oc{\'e}an-atmosph{\`e}re}},1757 author = { Guy Caniaux and Hervé Giordani and Jean-Luc Redelsperger and Malick Wade and Bernard Bourlès and Denis Bourras and Gaëlle De Coëtlogon and Yves Du Penhoat and Serge Janicot and Erica Key and Urbain Koffi and Nicolas Kolodziejczyk and Laurence Eymard and Julien Jouanno and Alban Lazar and Marion Leduc-Leballeur and Nathalie Lefèvre and Frédéric Marin and Hanh Nguyen and Gaëlle Parard},1758 abstract = {{The results gathered since the AMMA/EGEE campaigns of 2005-2007 in the field of air-sea interactions are presented. They show the key role of the Atlantic cold tongue (ACT) in the eastern equatorial Atlantic on the West African monsoon. The strengthening of south easterlies, associated with the Saint-Helena anticyclone, promotes the preconditioning of the thermocline along the equator and the development of the ACT.The equatorial front on its northern boundary, modifies the surface heat fluxes that affect the circulation in the lower atmosphere. This circulation helps to push moisture northward, toward the West African sub-continent, and impacts the monsoon jump.}},1759 keywords = { Mousson; Interaction oc{\'e}an-atmosph{\`e}re; Mod{\`e}le coupl{\'e} oc{\'e}an-atmosph{\`e}re; Pr{\'e}cipitations; Campagne de mesure; Afrique; Atlantique afrique ouest; Donn{\'e}es m{\'e}t{\'e}orologiques; Donn{\'e}es oc{\'e}anographiques; Circulation g{\'e}n{\'e}rale oc{\'e}anique; Equateur; Aliz{\'e}s; Convection; Thermocline; Sainte Helene; Anticyclone; Courant marin; Temp{\'e}rature de la mer; SST; Flux vertical; Flux d'interface; Circulation g{\'e}n{\'e}rale},1760 language = { Fran{\c c}ais},1761 affiliation = { Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME , Laboratoire de physique des oc{\'e}ans - LPO , Laboratoire de physique de l'atmosph{\`e}re et de l'oc{\'e}an Sim{\'e}on-Fongang - LPAOSF , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS , Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , National Science Foundation , Laboratoire de Physique de l'Atmosph{\`e}re, Universit{\'e} de Cocody - LAPA , Centro de Investigaci{\'o}n Cient{\'\i}fica y de Educaci{\'o}n Superior de Ensenada - CICESE , Department of Atmospheric and Environmental Sciences},1753 title = {{Les avancées d'AMMA sur les interactions océan-atmosphère}}, 1754 author = {{G}uy {C}aniaux and {H}ervé {G}iordani and {J}ean-{L}uc {R}edelsperger and {M}alick {W}ade and {B}ernard {B}ourlès and {D}enis {B}ourras and {G}aëlle {D}e {C}oëtlogon and {Y}ves {D}u {P}enhoat and {S}erge {J}anicot and {E}rica {K}ey and {U}rbain {K}offi and {N}icolas {K}olodziejczyk and {L}aurence {E}ymard and {J}ulien {J}ouanno and {A}lban {L}azar and {M}arion {L}educ-{L}eballeur and {N}athalie {L}efèvre and {F}rédéric {M}arin and {H}anh {N}guyen and {G}aëlle {P}arard}, 1755 abstract = {{The results gathered since the AMMA/EGEE campaigns of 2005-2007 in the field of air-sea interactions are presented. {T}hey show the key role of the {A}tlantic cold tongue (ACT) in the eastern equatorial {A}tlantic on the {W}est {A}frican monsoon. {T}he strengthening of south easterlies, associated with the {S}aint-{H}elena anticyclone, promotes the preconditioning of the thermocline along the equator and the development of the ACT. The equatorial front on its northern boundary, modifies the surface heat fluxes that affect the circulation in the lower atmosphere. {T}his circulation helps to push moisture northward, toward the {W}est {A}frican sub-continent, and impacts the monsoon jump.}}, 1756 keywords = {{M}ousson; {I}nteraction océan-atmosphère; {M}odèle couplé océan-atmosphère; {P}récipitations; {C}ampagne de mesure; {A}frique; {A}tlantique afrique ouest; {D}onnées météorologiques; {D}onnées océanographiques; {C}irculation générale océanique; {E}quateur; {A}lizés; {C}onvection; {T}hermocline; {S}ainte {H}elene; {A}nticyclone; {C}ourant marin; {T}empérature de la mer; SST; {F}lux vertical; {F}lux d'interface; {C}irculation générale}, 1757 language = {{F}rançais}, 1758 affiliation = {{G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME , {L}aboratoire de physique des océans - LPO , {L}aboratoire de physique de l'atmosphère et de l'océan {S}iméon-{F}ongang - LPAOSF , {L}aboratoire d'études en {G}éophysique et océanographie spatiales - LEGOS , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {N}ational {S}cience {F}oundation , {L}aboratoire de {P}hysique de l'{A}tmosphère, {U}niversité de {C}ocody - LAPA , {C}entro de {I}nvestigación {C}ientìfica y de {E}ducación {S}uperior de {E}nsenada - CICESE , {D}epartment of {A}tmospheric and {E}nvironmental {S}ciences}, 1762 1759 pages = {17-24}, 1763 journal = { La M{\'e}t{\'e}orologie},1764 number = { Octobre, Sp{\'e}cial AMMA},1760 journal = {{L}a {M}étéorologie}, 1761 number = {{O}ctobre, {S}pécial AMMA}, 1765 1762 audience = {internationale}, 1766 1763 doi = {10.4267/2042/48128}, … … 1775 1772 loceanaffectation={cnrs}, 1776 1773 title = {{L'observation spatiale dans le programme}}, 1777 author = {{L}aurence {E}ymard and Christian Baron and Guy Caniaux and Cyrille Flamant and Laurent Kergoat and Fatima Karbou and Jacques-André Ndione and Thierry Pellarin and Nadège Martiny and Johanna Ramarohetra and Elodie Vintrou and Rémy Roca},1778 abstract = {{Spaceborne Earth observation has been widely used within the AMMA program, for various studies: process, climate variability, society impact applications. Studies are being performed in the atmosphere, ocean, land surface domains as well as interactions between them. However, the AMMA experimental framework has offered the opportunity to develop space data methodologies: data validation of new sensors, specific regional validation benefiting from an exceptional data set, unusual in this region, development of new methodologies to get either variables more accurately (e.g. precipitations) or to exploit long-term series.}},1779 keywords = { Mousson; T{\'e}l{\'e}d{\'e}tection satellitaire; Afrique; Ouest; Lidar; A{\'e}rosol naturel; Poussi{\`e}re d'origine g{\'e}ologique; Humidit{\'e} du sol; Pr{\'e}cipitations; S{\'e}cheresse; Interaction sol-atmosph{\`e}re; Variabilit{\'e}; Campagne de mesure; S{\'e}ries chronologiques; Analyse des s{\'e}ries temporelles; Contr{\^o}le de l'instrument},1780 language = { Fran{\c c}ais},1781 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Territoires, Environnement, T{\'e}l{\'e}d{\'e}tection et Information Spatiale - UMR TETIS , Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME , Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Universit{\'e} Paris 6, Pierre et Marie Curie - UPMC , G{\'e}osciences Environnement Toulouse - GET , Laboratoire d'{\'e}tude des transferts en hydrologie et environnement - LTHE , Biog{\'e}osciences , Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD},1774 author = {{L}aurence {E}ymard and {C}hristian {B}aron and {G}uy {C}aniaux and {C}yrille {F}lamant and {L}aurent {K}ergoat and {F}atima {K}arbou and {J}acques-{A}ndré {N}dione and {T}hierry {P}ellarin and {N}adège {M}artiny and {J}ohanna {R}amarohetra and {E}lodie {V}introu and {R}émy {R}oca}, 1775 abstract = {{Spaceborne {E}arth observation has been widely used within the AMMA program, for various studies: process, climate variability, society impact applications. {S}tudies are being performed in the atmosphere, ocean, land surface domains as well as interactions between them. {H}owever, the AMMA experimental framework has offered the opportunity to develop space data methodologies: data validation of new sensors, specific regional validation benefiting from an exceptional data set, unusual in this region, development of new methodologies to get either variables more accurately (e.g. precipitations) or to exploit long-term series.}}, 1776 keywords = {{M}ousson; {T}élédétection satellitaire; {A}frique; {O}uest; {L}idar; {A}érosol naturel; {P}oussière d'origine géologique; {H}umidité du sol; {P}récipitations; {S}écheresse; {I}nteraction sol-atmosphère; {V}ariabilité; {C}ampagne de mesure; {S}éries chronologiques; {A}nalyse des séries temporelles; {C}ontrôle de l'instrument}, 1777 language = {{F}rançais}, 1778 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {T}erritoires, {E}nvironnement, {T}élédétection et {I}nformation {S}patiale - UMR TETIS , {G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {U}niversité {P}aris 6, {P}ierre et {M}arie {C}urie - UPMC , {G}éosciences {E}nvironnement {T}oulouse - GET , {L}aboratoire d'étude des transferts en hydrologie et environnement - LTHE , {B}iogéosciences , {L}aboratoire de {M}étéorologie {D}ynamique - LMD}, 1782 1779 pages = {80-89}, 1783 journal = { La M{\'e}t{\'e}orologie},1784 number = { Octobre, Sp{\'e}cial AMMA},1780 journal = {{L}a {M}étéorologie}, 1781 number = {{O}ctobre, {S}pécial AMMA}, 1785 1782 audience = {internationale}, 1786 1783 doi = {10.4267/2042/48136}, … … 1792 1789 loceanbibid = {01809}, 1793 1790 timestamp={20121012}, 1794 title = {{A fifty-year climatic signal in three Holocene stalagmite records from Mato Grosso, Brazil}},1795 author = { F. Soubiès and A. Seidel and A. Mangin and D. Genty and Josyane Ronchail and V. Plagnes and S. Hirooka and R. Santos},1796 language = { Anglais},1797 affiliation = { Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Instituto de Geoci{\^e}ncias , Laboratoire d'{\'e}cologie des hydrosyst{\`e}mes - LEH , Laboratoire des sciences du climat et de l'environnement - LSCE , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , ECOSS, Instituto Ecosistemas e Popula{\c c}{\\~o}es Tradicionais},1791 title = {{A fifty-year climatic signal in three {H}olocene stalagmite records from {M}ato {G}rosso, {B}razil}}, 1792 author = {{F}. {S}oubiès and A. {S}eidel and A. {M}angin and D. {G}enty and {J}osyane {R}onchail and V. {P}lagnes and S. {H}irooka and R. {S}antos}, 1793 language = {{A}nglais}, 1794 affiliation = {{P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {I}nstituto de {G}eociências , {L}aboratoire d'écologie des hydrosystèmes - LEH , {L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , ECOSS, {I}nstituto {E}cosistemas e {P}opulações {T}radicionais}, 1798 1795 pages = {115-129}, 1799 journal = { Quaternary International},1796 journal = {{Q}uaternary {I}nternational}, 1800 1797 volume = {135(1)}, 1801 audience = {non sp {\'e}cifi{\'e}e},1798 audience = {non spécifiée}, 1802 1799 doi = {10.1016/j.quaint.2004.10.027}, 1803 1800 year = {2005}, … … 1809 1806 timestamp={20121012}, 1810 1807 title = {{In-situ based pseudo-wind stress products for the tropical oceans}}, 1811 author = { Jacques Servain and S. Smith and David M. Legler and J. N. Stricherz and M. Bourassa and James J. O'Brien},1812 language = { Anglais},1813 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1808 author = {{J}acques {S}ervain and S. {S}mith and {D}avid M. {L}egler and J. N. {S}tricherz and M. {B}ourassa and {J}ames J. O'{B}rien}, 1809 language = {{A}nglais}, 1810 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1814 1811 pages = {979-994}, 1815 journal = { Bulletin of American Meteorological Society},1812 journal = {{B}ulletin of {A}merican {M}eteorological {S}ociety}, 1816 1813 volume = {85}, 1817 1814 number = {7}, … … 1825 1822 timestamp={20121012}, 1826 1823 title = {{Times-scales of variability from the high frequency PIRATA data revealed by wavelet analysis}}, 1827 author = { Jacques Servain and Gabriel Clauzet and Ilana Wainer},1828 language = { Anglais},1829 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},1824 author = {{J}acques {S}ervain and {G}abriel {C}lauzet and {I}lana {W}ainer}, 1825 language = {{A}nglais}, 1826 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1830 1827 pages = {43-58}, 1831 journal = { Brazilian Journal of Meteorology},1828 journal = {{B}razilian {J}ournal of {M}eteorology}, 1832 1829 volume = {20}, 1833 1830 number = {1}, … … 1840 1837 loceanbibid = {01806}, 1841 1838 timestamp={20121012}, 1842 title = {{On the connection between the 1984 Atlantic warm event the 1982-1983 ENSO}},1843 author = { Pascale Delecluse and Jacques Servain and Claire L{\'e}vy and K. Arpe and L. Bengtsson},1844 language = { Anglais},1845 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1839 title = {{On the connection between the 1984 {A}tlantic warm event the 1982-1983 ENSO}}, 1840 author = {{P}ascale {D}elecluse and {J}acques {S}ervain and {C}laire {L}évy and K. {A}rpe and L. {B}engtsson}, 1841 language = {{A}nglais}, 1842 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1846 1843 pages = {448-464}, 1847 journal = { Tellus Series A : Dynamic meteorology and oceanography},1844 journal = {{T}ellus {S}eries A : {D}ynamic meteorology and oceanography}, 1848 1845 volume = {46}, 1849 1846 number = {4}, 1850 audience = {non sp {\'e}cifi{\'e}e},1847 audience = {non spécifiée}, 1851 1848 doi = {10.1034/j.1600-0870.1994.t01-1-00009.x}, 1852 1849 year = {1994}, … … 1859 1856 loceanteam={phybiocar}, 1860 1857 loceanaffectation={cnrs}, 1861 title = {{Eddy properties in the California Current System}},1862 author = { Jaison Kurian and Francois Colas and Xavier Capet and James C. Macwilliams and Duddley B. Chelton},1863 abstract = {{Eddy detection and tracking algorithms are applied to both satellite altimetry and a high-resolution (dx = 5 km) climatological model solution of the U.S. West Coast to study the properties of surface and undercurrent eddies in the California Current System. Eddy properties show remarkable similarity in space and time, and even somewhat in polarity. Summer and fall are the most active seasons for undercurrent eddy generation, while there is less seasonal variation at surface. Most of the eddies have radii in the range of 25-100 km, sea level anomaly amplitudes of 1-4 cm, and vorticity normalized by f amplitudes of 0.025-0.2. Many of the eddies formed near the coast travel considerable distance westward with speeds about 2 km/day, consistent with the $\beta$ effect. Anticyclones and cyclones show equatorward and poleward displacements, respectively. Long-lived surface eddies show a cyclonic dominance. The subsurface California Undercurrent generates more long-lived anticyclones than cyclones through instabilities and topographic/coastline effects. In contrast, surface eddies and subsurface cyclones have much more widely distributed birth sites. The majority of the identified eddies have lifetimes less than a season. Eddies extend to 800-1500 m depth and have distinctive vertical structures for cyclones and anticyclones. Eddies show high nonlinearity (rotation speed higher than propagation speed) and hence can be efficient in transporting materials offshore.}},1864 language = { Anglais},1865 affiliation = { Institute of Geophysics and Planetary Physics [Los Angeles] - IGPP , Laboratoire de physique des oc{\'e}ans - LPO , College of Oceanic and Atmospheric Sciences},1858 title = {{Eddy properties in the {C}alifornia {C}urrent {S}ystem}}, 1859 author = {{J}aison {K}urian and {F}rancois {C}olas and {X}avier {C}apet and {J}ames C. {M}acwilliams and {D}uddley B. {C}helton}, 1860 abstract = {{Eddy detection and tracking algorithms are applied to both satellite altimetry and a high-resolution (dx = 5 km) climatological model solution of the U.S. {W}est {C}oast to study the properties of surface and undercurrent eddies in the {C}alifornia {C}urrent {S}ystem. {E}ddy properties show remarkable similarity in space and time, and even somewhat in polarity. {S}ummer and fall are the most active seasons for undercurrent eddy generation, while there is less seasonal variation at surface. {M}ost of the eddies have radii in the range of 25-100 km, sea level anomaly amplitudes of 1-4 cm, and vorticity normalized by f amplitudes of 0.025-0.2. {M}any of the eddies formed near the coast travel considerable distance westward with speeds about 2 km/day, consistent with the $\beta$ effect. {A}nticyclones and cyclones show equatorward and poleward displacements, respectively. {L}ong-lived surface eddies show a cyclonic dominance. {T}he subsurface {C}alifornia {U}ndercurrent generates more long-lived anticyclones than cyclones through instabilities and topographic/coastline effects. {I}n contrast, surface eddies and subsurface cyclones have much more widely distributed birth sites. {T}he majority of the identified eddies have lifetimes less than a season. {E}ddies extend to 800-1500 m depth and have distinctive vertical structures for cyclones and anticyclones. {E}ddies show high nonlinearity (rotation speed higher than propagation speed) and hence can be efficient in transporting materials offshore.}}, 1861 language = {{A}nglais}, 1862 affiliation = {{I}nstitute of {G}eophysics and {P}lanetary {P}hysics [Los {A}ngeles] - IGPP , {L}aboratoire de physique des océans - LPO , {C}ollege of {O}ceanic and {A}tmospheric {S}ciences}, 1866 1863 pages = {C08027}, 1867 journal = { Journal Of Geophysical Research Oceans},1864 journal = {{J}ournal {O}f {G}eophysical {R}esearch {O}ceans}, 1868 1865 volume = {116}, 1869 1866 audience = {internationale}, … … 1876 1873 loceanbibid = {01804}, 1877 1874 timestamp={20121012}, 1878 title = {{Life at cold seeps : a synthesis of biogeochemical and ecological data from Kazan mud volcano, eastern Mediterranean Sea}},1879 author = { Josef P. Werne and Ralf R. Haese and Tiphaine Zitter and Giovanni Aloisi and Ionna Bouloubassi and Sander Heijs and Aline Fiala-Médioni and Richard D. Pancost and Jaap S. Sinninghe Damsté and Gert De Lange and Larry J. Forney and Jan C. Gottschal and Jean-Paul Foucher and Jean Mascle and John Woodside},1880 language = { Anglais},1881 affiliation = { Department of Marine Biogeochemistry and Toxicology - NIOZ , Department of Geochemistry Faculty of Earth Sciences , Department of Sedimentology and Marine Geology Faculty of Earth and Life Sciences , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire de Chimie et Biog{\'e}ochimie Marines , Department of Microbiology , Laboratoire d'oc{\'e}anographie biologique de Banyuls - LOBB , D{\'e}partement G{\'e}osciences Marines , G{\'e}oazur - GEOAZUR , Centre for Marine Earth Science},1875 title = {{Life at cold seeps : a synthesis of biogeochemical and ecological data from {K}azan mud volcano, eastern {M}editerranean {S}ea}}, 1876 author = {{J}osef P. {W}erne and {R}alf R. {H}aese and {T}iphaine {Z}itter and {G}iovanni {A}loisi and {I}onna {B}ouloubassi and {S}ander {H}eijs and {A}line {F}iala-{M}édioni and {R}ichard D. {P}ancost and {J}aap S. {S}inninghe {D}amsté and {G}ert {D}e {L}ange and {L}arry J. {F}orney and {J}an C. {G}ottschal and {J}ean-{P}aul {F}oucher and {J}ean {M}ascle and {J}ohn {W}oodside}, 1877 language = {{A}nglais}, 1878 affiliation = {{D}epartment of {M}arine {B}iogeochemistry and {T}oxicology - NIOZ , {D}epartment of {G}eochemistry {F}aculty of {E}arth {S}ciences , {D}epartment of {S}edimentology and {M}arine {G}eology {F}aculty of {E}arth and {L}ife {S}ciences , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire de {C}himie et {B}iogéochimie {M}arines , {D}epartment of {M}icrobiology , {L}aboratoire d'océanographie biologique de {B}anyuls - LOBB , {D}épartement {G}éosciences {M}arines , {G}éoazur - GEOAZUR , {C}entre for {M}arine {E}arth {S}cience}, 1882 1879 pages = {367-390}, 1883 journal = { Chemical Geology},1880 journal = {{C}hemical {G}eology}, 1884 1881 volume = {205}, 1885 1882 audience = {internationale}, … … 1891 1888 loceanbibid = {01803}, 1892 1889 timestamp={20121012}, 1893 title = {{Lipids and their modes of occurence in two surface sediments from the Danube delta and northwestern Black sea. Implications for sources and early diagenetic alterations. I. Carboxylics acids.}},1894 author = { A. Garcette-Lepecq and C. Largeau and Ioanna Bouloubassi and S. Derenne and Alain Saliot and Anne Lorre and V. Point},1895 language = { Anglais},1896 affiliation = { Biog{\'e}ochimie et {\'e}cologie des milieux continentaux - Bioemco},1890 title = {{Lipids and their modes of occurence in two surface sediments from the {D}anube delta and northwestern {B}lack sea. {I}mplications for sources and early diagenetic alterations. I. {C}arboxylics acids.}}, 1891 author = {{A}. {G}arcette-{L}epecq and C. {L}argeau and {I}oanna {B}ouloubassi and S. {D}erenne and {A}lain {S}aliot and {A}nne {L}orre and V. {P}oint}, 1892 language = {{A}nglais}, 1893 affiliation = {{B}iogéochimie et écologie des milieux continentaux - {B}ioemco}, 1897 1894 pages = {959-980}, 1898 journal = { Org. geochem.},1895 journal = {{O}rg. geochem.}, 1899 1896 volume = {35}, 1900 audience = {non sp {\'e}cifi{\'e}e},1897 audience = {non spécifiée}, 1901 1898 year = {2004}, 1902 1899 } … … 1907 1904 timestamp={20121012}, 1908 1905 title = {{CH4-consuming microorganisms and the formation of carbonate crusts at cold-seeps}}, 1909 author = { Giovanni Aloisi and Ioanna Bouloubassi and Sander Heijs and Richard Pancost and Catherine Pierre and Damst{\'e} Jaap S. Sinninghe and Jan C. Gottschaland Larry J. Forney and J.-M. Rouchy},1910 language = { Anglais},1911 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire de biog{\'e}ochimie et chimie marines - LBCM},1906 author = {{G}iovanni {A}loisi and {I}oanna {B}ouloubassi and {S}ander {H}eijs and {R}ichard {P}ancost and {C}atherine {P}ierre and {D}amsté {J}aap S. {S}inninghe and {J}an C. {G}ottschaland {L}arry J. {F}orney and J.-{M}. {R}ouchy}, 1907 language = {{A}nglais}, 1908 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire de biogéochimie et chimie marines - LBCM}, 1912 1909 pages = {195-203}, 1913 journal = { Earth and Planetary Science Letters},1910 journal = {{E}arth and {P}lanetary {S}cience {L}etters}, 1914 1911 volume = {203}, 1915 audience = {non sp {\'e}cifi{\'e}e},1912 audience = {non spécifiée}, 1916 1913 year = {2002}, 1917 1914 comment = {20121114 : doublon hal-00170824}, … … 1922 1919 hal_id = {hal-00310889}, 1923 1920 timestamp={20121012}, 1924 title = {{Hydrology and circulation in the Strait of Hormuz and the Gulf of Oman-Results from the GOGP99 Experiment: 2. Gulf of Oman.}},1925 author = {{S}téphane {P}ous and X. Carton and P. Lazure},1926 abstract = {{Hydrological, ADCP, and drifting buoy data obtained during the GOGP99 Experiment in October and early November 1999 are analyzed to describe the Persian Gulf Water (PGW) core and the regional circulation in the Gulf of Oman. The warm and salty PGW core flows out of the Strait of Hormuz heading southeastward unto (25°20#N, 57°E), approximately. From there, it cascades down the continental slope, veers southwestward, and joins the Omani coast near (24°50#N, 56°50#E) to form a slope current. This PGW current has then thermohaline maxima on isopycnal $\sigma$0 = 26.5, near 220 m depth. Its thermohaline characteristics decrease along its progression to Ra's al Hadd (and then offshore into the Arabian Sea) but maintain a sharp contrast with surrounding waters. Outflow variability at the Strait of Hormuz can be related to downstream fluctuations of the thermohaline maxima in the PGW core at gulf scale and over a 2- to 3-week period. Moreover, several mechanisms (baroclinic instability, flow intermittency, cape effects) are examined to explain the widening of this PGW core upstream and downstream of Ra's al Hamra. In the eastern part of the Gulf of Oman, the regional circulation is a cyclonic gyre. The circulation in the western part of the Gulf is more complex, with the outflow of PGW and southeastward currents in the upper 250 m near the Omani coast, and a recirculation of upwelled waters near Ra's Jagin (on the Iranian coast). The large cyclonic gyre occupies at least the upper 300 m of the water column and undergoes little variation over a month. The PGW outflow in the northern Arabian Sea is southward and located 50--100 km from the coast. It borders a shallower northward current located offshore.}},1927 keywords = { Gulf of Oman; regional circulation; Persian Gulf Water outflow.},1928 language = { Anglais},1929 affiliation = { Laboratoire de physique des oc{\'e}ans - LPO , Direction de l'Environnement et de l'am{\'e}nagement Littoral},1921 title = {{Hydrology and circulation in the {S}trait of {H}ormuz and the {G}ulf of {O}man-{R}esults from the GOGP99 {E}xperiment: 2. {G}ulf of {O}man.}}, 1922 author = {{S}téphane {P}ous and X. {C}arton and P. {L}azure}, 1923 abstract = {{Hydrological, ADCP, and drifting buoy data obtained during the GOGP99 {E}xperiment in {O}ctober and early {N}ovember 1999 are analyzed to describe the {P}ersian {G}ulf {W}ater (PGW) core and the regional circulation in the {G}ulf of {O}man. {T}he warm and salty PGW core flows out of the {S}trait of {H}ormuz heading southeastward unto (25°20#N, 57°E), approximately. {F}rom there, it cascades down the continental slope, veers southwestward, and joins the {O}mani coast near (24°50#N, 56°50#E) to form a slope current. {T}his PGW current has then thermohaline maxima on isopycnal $\sigma$0 = 26.5, near 220 m depth. {I}ts thermohaline characteristics decrease along its progression to {R}a's al {H}add (and then offshore into the {A}rabian {S}ea) but maintain a sharp contrast with surrounding waters. {O}utflow variability at the {S}trait of {H}ormuz can be related to downstream fluctuations of the thermohaline maxima in the PGW core at gulf scale and over a 2- to 3-week period. {M}oreover, several mechanisms (baroclinic instability, flow intermittency, cape effects) are examined to explain the widening of this PGW core upstream and downstream of {R}a's al {H}amra. {I}n the eastern part of the {G}ulf of {O}man, the regional circulation is a cyclonic gyre. {T}he circulation in the western part of the {G}ulf is more complex, with the outflow of PGW and southeastward currents in the upper 250 m near the {O}mani coast, and a recirculation of upwelled waters near {R}a's {J}agin (on the {I}ranian coast). {T}he large cyclonic gyre occupies at least the upper 300 m of the water column and undergoes little variation over a month. {T}he PGW outflow in the northern {A}rabian {S}ea is southward and located 50--100 km from the coast. {I}t borders a shallower northward current located offshore.}}, 1924 keywords = {{G}ulf of {O}man; regional circulation; {P}ersian {G}ulf {W}ater outflow.}, 1925 language = {{A}nglais}, 1926 affiliation = {{L}aboratoire de physique des océans - LPO , {D}irection de l'{E}nvironnement et de l'aménagement {L}ittoral}, 1930 1927 pages = {C12038}, 1931 journal = { Journal of Geophysical Research C: Oceans},1928 journal = {{J}ournal of {G}eophysical {R}esearch C: {O}ceans}, 1932 1929 volume = {109}, 1933 1930 audience = {internationale}, … … 1940 1937 loceanbibid = {01800}, 1941 1938 timestamp={20121012}, 1942 title = {{Hydrology and circulation in the Strait of Hormuz and the Gulf of Oman-Results from the GOGP99 Experiment: 1. Strait of Hormuz}},1943 author = {{S}téphane {P}ous and X. Carton and P. Lazure},1944 abstract = {{In October and early November 1999, the GOGP99 experiment collected hydrological, currentmeter, tide recorder, thermistor and drifting buoy data near the Strait of Hormuz. Data analysis provides the water mass structure in the Strait: Persian Gulf Water (PGW) core is banked against the Omani coast, while Indian Ocean Surface Water (IOSW) lies near the Iranian coast. These water masses are most often covered by a homogeneous surface layer. Thermohaline characteristics of the PGW core decrease substantially downstream, from the Persian/Arabian Gulf to the Gulf of Oman. PGW and IOSW thermohaline characteristics and distribution also exhibit notable changes at periods shorter than a month as shown by repeated hydrological sections. The tidal signal measured south of the Strait by moored ADCP and thermistor chains has predominant semi-diurnal M2 and S2 and diurnal K1 components and possesses a complex vertical structure. Tidal intensification near the surface pycnocline is associated with noticeable internal waves. At subtidal timescale, mooring recordings confirm the water mass variability observed in the repeated hydrological sections. The mixed layer also deepens substantially during the 1-month period. Finally, trajectories of surface buoys drogued at 15 m exhibit reversals over periods characteristic of changes in wind direction.}},1945 keywords = { Hormuz; hydrology.},1946 language = { Anglais},1947 affiliation = { Laboratoire de physique des oc{\'e}ans - LPO , Direction de l'Environnement et de l'am{\'e}nagement Littoral},1939 title = {{Hydrology and circulation in the {S}trait of {H}ormuz and the {G}ulf of {O}man-{R}esults from the GOGP99 {E}xperiment: 1. {S}trait of {H}ormuz}}, 1940 author = {{S}téphane {P}ous and X. {C}arton and P. {L}azure}, 1941 abstract = {{In {O}ctober and early {N}ovember 1999, the GOGP99 experiment collected hydrological, currentmeter, tide recorder, thermistor and drifting buoy data near the {S}trait of {H}ormuz. {D}ata analysis provides the water mass structure in the {S}trait: {P}ersian {G}ulf {W}ater (PGW) core is banked against the {O}mani coast, while {I}ndian {O}cean {S}urface {W}ater (IOSW) lies near the {I}ranian coast. {T}hese water masses are most often covered by a homogeneous surface layer. {T}hermohaline characteristics of the PGW core decrease substantially downstream, from the {P}ersian/Arabian {G}ulf to the {G}ulf of {O}man. PGW and IOSW thermohaline characteristics and distribution also exhibit notable changes at periods shorter than a month as shown by repeated hydrological sections. {T}he tidal signal measured south of the {S}trait by moored ADCP and thermistor chains has predominant semi-diurnal M2 and S2 and diurnal K1 components and possesses a complex vertical structure. {T}idal intensification near the surface pycnocline is associated with noticeable internal waves. {A}t subtidal timescale, mooring recordings confirm the water mass variability observed in the repeated hydrological sections. {T}he mixed layer also deepens substantially during the 1-month period. {F}inally, trajectories of surface buoys drogued at 15 m exhibit reversals over periods characteristic of changes in wind direction.}}, 1942 keywords = {{H}ormuz; hydrology.}, 1943 language = {{A}nglais}, 1944 affiliation = {{L}aboratoire de physique des océans - LPO , {D}irection de l'{E}nvironnement et de l'aménagement {L}ittoral}, 1948 1945 pages = {C12037}, 1949 journal = { Journal of Geophysical Research C: Oceans},1946 journal = {{J}ournal of {G}eophysical {R}esearch C: {O}ceans}, 1950 1947 volume = {109}, 1951 1948 audience = {internationale}, … … 1961 1958 timestamp={20121012}, 1962 1959 author = {{M}arion {L}educ-{L}eballeur and {L}aurence {E}ymard and {G}aëlle {{d}e {C}oëtlogon}}, 1963 title = { Air-sea interaction in the Gulf of Guinea at intraseasonal timescales: wind bursts and coastal precipitation in boreal spring},1964 language = { Anglais},1960 title = { Air-sea interaction in the {G}ulf of {G}uinea at intraseasonal timescales: wind bursts and coastal precipitation in boreal spring}, 1961 language = {{A}nglais}, 1965 1962 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {U}niversité {P}aris 6, {P}ierre et {M}arie {C}urie - UPMC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 1966 1963 booktitle = {4th {AMMA} {I}nternational {C}onference}, … … 1974 1971 loceanbibid = {01798}, 1975 1972 timestamp = {20121109}, 1976 title = {{Use of a Neurovariational Inversion for Retrieving Oceanic and Atmospheric Constituents from Ocean Color Imagery: A Feasibility Study}},1977 author = { C. Jamet and {S}ylvie {T}hiria and C. Moulin and {M}ichel {C}répon},1978 language = { Anglais},1979 affiliation = { Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , ACRI-ST - ACRI-ST , Laboratoire des sciences du climat et de l'environnement - LSCE},1973 title = {{Use of a {N}eurovariational {I}nversion for {R}etrieving {O}ceanic and {A}tmospheric {C}onstituents from {O}cean {C}olor {I}magery: A {F}easibility {S}tudy}}, 1974 author = {{C}. {J}amet and {S}ylvie {T}hiria and C. {M}oulin and {M}ichel {C}répon}, 1975 language = {{A}nglais}, 1976 affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , ACRI-ST - ACRI-ST , {L}aboratoire des sciences du climat et de l'environnement - LSCE}, 1980 1977 pages = {460-475}, 1981 journal = { Journal of Atmospheric and Oceanic Technology},1978 journal = {{J}ournal of {A}tmospheric and {O}ceanic {T}echnology}, 1982 1979 volume = {22}, 1983 audience = {non sp {\'e}cifi{\'e}e},1980 audience = {non spécifiée}, 1984 1981 doi = {10.1175/JTECH1688.1}, 1985 1982 year = {2005}, … … 1992 1989 loceanaffectation={cnrs}, 1993 1990 title = {{Mean circulations and variability between 1958 and 2004 as simulated by the DAKKAR eddy permitting 1\/4° global ocean/sea ice model driven by CORE or ERA40 atmospheric forcing}}, 1994 author = {{B}ernard {B}arnier and {T}hierry {P}enduff and {J}ean-{M}arc {M}olines and {A}nne-{M}arie {T}réguier and Arne Biastoch and {G}urvan {M}adec and Claus Böning},1995 language = { Anglais},1996 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , IfM-GEOMAR , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC},1997 booktitle = {{Proc. EGU General Assembly}},1998 pages = {pas pr {\'e}cise},1999 address = {vienne, France},1991 author = {{B}ernard {B}arnier and {T}hierry {P}enduff and {J}ean-{M}arc {M}olines and {A}nne-{M}arie {T}réguier and {A}rne {B}iastoch and {G}urvan {M}adec and {C}laus {B}öning}, 1992 language = {{A}nglais}, 1993 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {I}fM-GEOMAR , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 1994 booktitle = {{Proc. EGU {G}eneral {A}ssembly}}, 1995 pages = {pas précise}, 1996 address = {vienne, {F}rance}, 2000 1997 audience = {internationale}, 2001 1998 year = {2007}, … … 2007 2004 loceanbibid = {01796}, 2008 2005 timestamp = {20121108}, 2009 title = {{Validation of Sea Level Data in the East Asian Marginal Seas: Comparison between TOPEX/POSEIDON Altimeter and In-Situ Tide Gauges}},2010 author = { Y.-H. Youn and I. S. Oh and K.-H. Kim and {Y}oung-{H}yang {P}ark and J. W. Kim},2011 abstract = {{In an effort to assess the reliability of satellite altimeter systems, the authors conduct a comparative analysis of sea level data that were collected from the TOPEX/POSEIDON (T/P) altimeter and 10 tide gauges (TG) near the satellite passing ground tracks. The analysis is made using datasets collected from marginal sea regions surrounding the Korean Peninsula at T/P cycles of 2 to 230, which correspond to October 1992 to December 1998. Proper treatment of tidal errors is a very critical step in data processing because the study area has very strong tide. When the T/P data are processed, the procedures of Park and Gamberoni (1995) are adapted to reduce errors associated with the tide. When the T/P data are processed in this way, the alias periods of M2, S2, and K1 constituents are found to be 62.1, 58.7, and 173 days repectively. The compatibility of the T/P and TG datasets are examined at various filtering periods. The results indicate that the low-frequency signals of the T/P data can be interpreted more safely with longer filtering periods (such as up to the maximum selected value of 200 days). When RMS errors for the 200-day low-pass filter period are compared with all 10 tidal stations, the values span the range of 2.8 to 6.7 cm. The results of a correlation analysis for this filtering period also show a strong agreement between the T/P and TG datasets across all stations investigated (e.g., p-values consistently less than 0.001). Hence according to the analysis, the conclusion is made that the analysis of surface sea level using satellite altimeter data can be made safely with reasonably extended filtering periods such as 200 days.}},2012 language = { Anglais},2013 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2006 title = {{Validation of {S}ea {L}evel {D}ata in the {E}ast {A}sian {M}arginal {S}eas: {C}omparison between TOPEX/POSEIDON {A}ltimeter and {I}n-{S}itu {T}ide {G}auges}}, 2007 author = {{Y}.-{H}. {Y}oun and I. S. {O}h and K.-{H}. {K}im and {Y}oung-{H}yang {P}ark and J. W. {K}im}, 2008 abstract = {{In an effort to assess the reliability of satellite altimeter systems, the authors conduct a comparative analysis of sea level data that were collected from the TOPEX/POSEIDON (T/P) altimeter and 10 tide gauges (TG) near the satellite passing ground tracks. {T}he analysis is made using datasets collected from marginal sea regions surrounding the {K}orean {P}eninsula at T/P cycles of 2 to 230, which correspond to {O}ctober 1992 to {D}ecember 1998. {P}roper treatment of tidal errors is a very critical step in data processing because the study area has very strong tide. {W}hen the T/P data are processed, the procedures of {P}ark and {G}amberoni (1995) are adapted to reduce errors associated with the tide. {W}hen the T/P data are processed in this way, the alias periods of M2, S2, and K1 constituents are found to be 62.1, 58.7, and 173 days repectively. {T}he compatibility of the T/P and TG datasets are examined at various filtering periods. {T}he results indicate that the low-frequency signals of the T/P data can be interpreted more safely with longer filtering periods (such as up to the maximum selected value of 200 days). {W}hen RMS errors for the 200-day low-pass filter period are compared with all 10 tidal stations, the values span the range of 2.8 to 6.7 cm. {T}he results of a correlation analysis for this filtering period also show a strong agreement between the T/P and TG datasets across all stations investigated (e.g., p-values consistently less than 0.001). {H}ence according to the analysis, the conclusion is made that the analysis of surface sea level using satellite altimeter data can be made safely with reasonably extended filtering periods such as 200 days.}}, 2009 language = {{A}nglais}, 2010 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2014 2011 pages = {650-660}, 2015 journal = { Advances in Atmospheric Sciences},2012 journal = {{A}dvances in {A}tmospheric {S}ciences}, 2016 2013 volume = {20}, 2017 2014 number = {4}, 2018 2015 note = {http://www.iap.ac.cn/html/qikan/aas/aas2003/200304/204yhy.pdf}, 2019 audience = {non sp {\'e}cifi{\'e}e},2016 audience = {non spécifiée}, 2020 2017 year = {2004}, 2021 2018 } … … 2027 2024 title = {{Determination of the surface geostrophic velocity field from satellite altimetry}}, 2028 2025 author = {{Y}oung-{H}yang {P}ark}, 2029 abstract = {{Determination of the surface geostrophic velocity field from satellite altimetryPresently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. With a given quasi-geostrophic balance for the horizontal surface flow, a scaling analysis of this boundary condition indicates that although the vertical velocity w is mostly balanced by the local change of the free surface, $\partial$$\eta$#/$\partial$t, useful information on the mean current (u overline, v overline) is contained in a small ageostrophic departure ($\partial$$\eta$#/$\partial$t -- w). Our method consists in the development of a simple algebraic equation with two unknowns (u overline, v overline) and an adjustable parameter inline equation associated with $\partial$$\eta$#/$\partial$t, assuming that the latter is proportional to ($\partial$$\eta$#/$\partial$t -- w). Most interestingly, $\partial$$\eta$#/$\partial$t and all other coefficients of the equation can be determined from altimetry. The altimeter data used is combined TOPEX/Poseidon-ERS gridded data, and the solution is obtained by least squares, minimizing the contribution from the time-variable part of the parameter inline equation and prescribing the zonal direction of the mean current. The method, which is found to be particularly useful for quasi-zonal high-energy current systems, has been validated against direct observations in the Gulf Stream and Southern Ocean. Comparisons with direct observations and Monte Carlo experiments suggest an overall solution error of about 10 cm s--1. Once calibrated against regional velocity statistics, this method will be able to determine from altimetry the mean or instantaneous surface velocity field down to the frontal scale, with a realism that has been inaccessible because of the geoid constraint.}},2030 language = { Anglais},2031 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2026 abstract = {{Determination of the surface geostrophic velocity field from satellite altimetryPresently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. {W}ith a given quasi-geostrophic balance for the horizontal surface flow, a scaling analysis of this boundary condition indicates that although the vertical velocity w is mostly balanced by the local change of the free surface, $\partial$$\eta$#/$\partial$t, useful information on the mean current (u overline, v overline) is contained in a small ageostrophic departure ($\partial$$\eta$#/$\partial$t -- w). {O}ur method consists in the development of a simple algebraic equation with two unknowns (u overline, v overline) and an adjustable parameter inline equation associated with $\partial$$\eta$#/$\partial$t, assuming that the latter is proportional to ($\partial$$\eta$#/$\partial$t -- w). {M}ost interestingly, $\partial$$\eta$#/$\partial$t and all other coefficients of the equation can be determined from altimetry. {T}he altimeter data used is combined TOPEX/Poseidon-ERS gridded data, and the solution is obtained by least squares, minimizing the contribution from the time-variable part of the parameter inline equation and prescribing the zonal direction of the mean current. {T}he method, which is found to be particularly useful for quasi-zonal high-energy current systems, has been validated against direct observations in the {G}ulf {S}tream and {S}outhern {O}cean. {C}omparisons with direct observations and {M}onte {C}arlo experiments suggest an overall solution error of about 10 cm s--1. {O}nce calibrated against regional velocity statistics, this method will be able to determine from altimetry the mean or instantaneous surface velocity field down to the frontal scale, with a realism that has been inaccessible because of the geoid constraint.}}, 2027 language = {{A}nglais}, 2028 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2032 2029 pages = {C05006}, 2033 journal = { Journal of Geophysical Research},2030 journal = {{J}ournal of {G}eophysical {R}esearch}, 2034 2031 volume = {109}, 2035 audience = {non sp {\'e}cifi{\'e}e},2032 audience = {non spécifiée}, 2036 2033 doi = {10.1029/2003JC002115}, 2037 2034 year = {2004}, … … 2042 2039 loceanbibid = {01794}, 2043 2040 timestamp = {20121108}, 2044 title = {{Nutrients and carbon budgets for the gulf of Lions during the MOGLI cruises}},2045 author = { Xavier Durrieu De Madron and L. Denis and Frederic Diaz and Nicole Garcia and Cécile Guieu and C. Grenz and Marie-Dominique Loÿe-Pilota and W. Ludwig and Thierry Moutin and Patrick Raimbault and Céline Ridame},2046 language = { Anglais},2047 affiliation = { Laboratoire d'oc{\'e}anographie et de biog{\'e}ochimie - LOB , Laboratoire d'oc{\'e}anographie de Villefranche - LOV , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2041 title = {{Nutrients and carbon budgets for the gulf of {L}ions during the MOGLI cruises}}, 2042 author = {{X}avier {D}urrieu {D}e {M}adron and L. {D}enis and {F}rederic {D}iaz and {N}icole {G}arcia and {C}écile {G}uieu and C. {G}renz and {M}arie-{D}ominique {L}oÿe-{P}ilota and W. {L}udwig and {T}hierry {M}outin and {P}atrick {R}aimbault and {C}éline {R}idame}, 2043 language = {{A}nglais}, 2044 affiliation = {{L}aboratoire d'océanographie et de biogéochimie - LOB , {L}aboratoire d'océanographie de {V}illefranche - LOV , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2048 2045 pages = {421-433}, 2049 journal = { Oceanologica Acta},2046 journal = {{O}ceanologica {A}cta}, 2050 2047 volume = {26}, 2051 2048 number = {4}, … … 2059 2056 timestamp = {20121108}, 2060 2057 loceanaffectation={cnrs}, 2061 title = {{The Brazil Malvinas Frontal System as seen from nine years of AVHRR data.}},2062 author = { M. Saraceno and {C}hristine {P}rovost and Alberto R. Piola and José Bava and Antonio Gagliardini},2063 language = { Anglais},2064 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2058 title = {{The {B}razil {M}alvinas {F}rontal {S}ystem as seen from nine years of AVHRR data.}}, 2059 author = {{M}. {S}araceno and {C}hristine {P}rovost and {A}lberto R. {P}iola and {J}osé {B}ava and {A}ntonio {G}agliardini}, 2060 language = {{A}nglais}, 2061 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2065 2062 pages = {C05027}, 2066 journal = { Journal of Geophysical Research C: Oceans},2063 journal = {{J}ournal of {G}eophysical {R}esearch C: {O}ceans}, 2067 2064 volume = {109}, 2068 2065 number = {C5}, 2069 audience = {non sp {\'e}cifi{\'e}e},2066 audience = {non spécifiée}, 2070 2067 doi = {10.1029/2003JC002127}, 2071 2068 year = {2004}, … … 2078 2075 timestamp = {20121108}, 2079 2076 loceanaffectation={cnrs}, 2080 title = {{Centennial to millennial-scale variability of the Indian monsoon during the early Holocene from a sediment, pollen and isotope record from the desert of Yemen}},2081 author = {{A}nne-{M}arie {L}ézine and J.- J. Tiercelin and C. Robert and {J}ean-{F}rançois {S}aliège and S. Cleuziou and M.-L. Inizan and F. Braemer},2082 abstract = {{Lacustrine deposits of al- Hawa (15°52#N, 46°53#E, 710 m above sea level) document the climatic and environmental history of the inland desert of Yemen during the early to mid-Holocene. A freshwater lake expanded in one of the most arid areas of the world in response to increased Indian monsoon fluxes from 12,000 to 7500 cal B.P. Three dry intervals punctuated the lacustrine phase recording episodes of weaker summer monsoon activity over Arabia. Dry intervals were coeval with cold periods recorded in the North Atlantic, confirming the links between the Indian monsoon and the North Atlantic systems during the Holocene. We demonstrate that the regional vegetation remained of semi-arid character throughout the lacustrine period.}},2083 keywords = { Pollen; Oxygen isotopes; Clay mineralogy; Paleolake; Yemen; Holocene},2084 language = { Anglais},2085 affiliation = { Laboratoire des sciences du climat et de l'environnement - LSCE , Domaines Oc{\'e}aniques , Processus et bilan des domaines s{\'e}dimentaires - PBDS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Arch{\'e}ologies et Sciences de l'Antiquit{\'e} - ArScAn , Pr{\'e}histoire et Technologie - PT , Centre d'{\'E}tudes Pr{\'e}histoire, Antiquit{\'e}, Moyen-Age - CEPAM},2077 title = {{Centennial to millennial-scale variability of the {I}ndian monsoon during the early {H}olocene from a sediment, pollen and isotope record from the desert of {Y}emen}}, 2078 author = {{A}nne-{M}arie {L}ézine and J.-{J}. {T}iercelin and C. {R}obert and {J}ean-{F}rançois {S}aliège and S. {C}leuziou and M.-{L}. {I}nizan and F. {B}raemer}, 2079 abstract = {{Lacustrine deposits of al-{H}awa (15°52#N, 46°53#E, 710 m above sea level) document the climatic and environmental history of the inland desert of {Y}emen during the early to mid-{H}olocene. A freshwater lake expanded in one of the most arid areas of the world in response to increased {I}ndian monsoon fluxes from 12,000 to 7500 cal B.P. {T}hree dry intervals punctuated the lacustrine phase recording episodes of weaker summer monsoon activity over {A}rabia. {D}ry intervals were coeval with cold periods recorded in the {N}orth {A}tlantic, confirming the links between the {I}ndian monsoon and the {N}orth {A}tlantic systems during the {H}olocene. {W}e demonstrate that the regional vegetation remained of semi-arid character throughout the lacustrine period.}}, 2080 keywords = {{P}ollen; {O}xygen isotopes; {C}lay mineralogy; {P}aleolake; {Y}emen; {H}olocene}, 2081 language = {{A}nglais}, 2082 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {D}omaines {O}céaniques , {P}rocessus et bilan des domaines sédimentaires - PBDS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {A}rchéologies et {S}ciences de l'{A}ntiquité - {A}rScAn , {P}réhistoire et {T}echnologie - PT , {C}entre d'Études {P}réhistoire, {A}ntiquité, {M}oyen-{A}ge - CEPAM}, 2086 2083 pages = {235-249}, 2087 journal = { Palaeogeography Palaeoclimatology Palaeoecology / Palaeogeography Palaeoclimatology and Palaeoecology},2084 journal = {{P}alaeogeography {P}alaeoclimatology {P}alaeoecology / {P}alaeogeography {P}alaeoclimatology and {P}alaeoecology}, 2088 2085 volume = {243}, 2089 2086 number = {3-4}, … … 2100 2097 loceanteam={surf}, 2101 2098 loceanaffectation={cnrs}, 2102 title = {{Overview of the SMOS Sea Surface Salinity Prototype Processor}},2099 title = {{Overview of the SMOS {S}ea {S}urface {S}alinity {P}rototype {P}rocessor}}, 2103 2100 author = {{S}onia {Z}ine and {J}acqueline {B}outin and {J}. {F}ont and {C}. {G}abarro and {M}. {T}alone and {N}. {R}eul and {J}. {T}enerelli and {Ph}ilippe {W}aldteufel and {F}. {P}etitcolin and {J}ean-{L}uc {V}ergely}, 2104 collaboration = {SMOS Collaboration(s)},2105 abstract = {{The Soil Moisture and Ocean Salinity (SMOS) mission (launch scheduled for 2008) aims at obtaining global maps of soil moisture and sea surface salinity (SSS). It uses an L-band (1.4 GHz) microwave interferometric radiometer to obtain brightness temperatures (Tb) at the Earth surface at horizontal and vertical polarizations. They will be used to retrieve both geophysical variables, following specifically designed algorithms that will be applied when the satellite field-of-view is covering land or ocean surfaces respectively. The retrieval of salinity is a complex process that requires the knowledge of environmental information and an accurate processing of the radiometer measurements, because of the narrow range of ocean Tb and the strong impact on the measures of geophysical parameters (such as sea state). Here we present the baseline approach chosen to retrieve sea surface salinity from SMOS data, as developed and implemented by the joint team of scientists and engineers responsible for the SMOS Salinity Level 2 Prototype Processor. We present academic tests conducted over homogeneous scenes with the prototype. In these configurations, external perturbation sources (sky radiation, sun glint, ...) are not taken into account. Roughness is the main sea surface signal disturbing SSS retrieval. In dual pol, wind speed biases are better corrected at the center of the swath than at the edge.}},2106 keywords = {SMOS Salinit{\'e}de surface},2107 language = { Anglais},2108 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Institut de Ci{\`e}nces del Mar - ICM , Laboratoire d'Oc{\'e}anographie Spatiale - LOS , Service d'a{\'e}ronomie - SA},2101 collaboration = {SMOS {C}ollaboration(s)}, 2102 abstract = {{The {S}oil {M}oisture and {O}cean {S}alinity (SMOS) mission (launch scheduled for 2008) aims at obtaining global maps of soil moisture and sea surface salinity (SSS). {I}t uses an L-band (1.4 GHz) microwave interferometric radiometer to obtain brightness temperatures (Tb) at the {E}arth surface at horizontal and vertical polarizations. {T}hey will be used to retrieve both geophysical variables, following specifically designed algorithms that will be applied when the satellite field-of-view is covering land or ocean surfaces respectively. {T}he retrieval of salinity is a complex process that requires the knowledge of environmental information and an accurate processing of the radiometer measurements, because of the narrow range of ocean {T}b and the strong impact on the measures of geophysical parameters (such as sea state). {H}ere we present the baseline approach chosen to retrieve sea surface salinity from SMOS data, as developed and implemented by the joint team of scientists and engineers responsible for the SMOS {S}alinity {L}evel 2 {P}rototype {P}rocessor. {W}e present academic tests conducted over homogeneous scenes with the prototype. {I}n these configurations, external perturbation sources (sky radiation, sun glint, ...) are not taken into account. {R}oughness is the main sea surface signal disturbing SSS retrieval. {I}n dual pol, wind speed biases are better corrected at the center of the swath than at the edge.}}, 2103 keywords = {SMOS {S}alinité de surface}, 2104 language = {{A}nglais}, 2105 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {I}nstitut de {C}iènces del {M}ar - ICM , {L}aboratoire d'{O}céanographie {S}patiale - LOS , {S}ervice d'aéronomie - SA}, 2109 2106 booktitle = {{IGARSS07 proceedings}}, 2110 pages = { Th07AF},2111 address = {BARCELONE, Espagne},2112 note = {TOSCA/SMOS ESL salinit {\'e}},2107 pages = {{T}h07AF}, 2108 address = {BARCELONE, {E}spagne}, 2109 note = {TOSCA/SMOS ESL salinité}, 2113 2110 audience = {internationale}, 2114 2111 collaboration = {SMOS}, … … 2122 2119 loceanbibid = {01789}, 2123 2120 timestamp = {20121108}, 2124 title = {{Optimal Surface Salinity Perturbations Influencing the Thermohaline Circulation.}},2125 author = {{F}lorian {S}évellec and Mahdi Ben Jelloul and Thierry Huck},2126 abstract = {{Optimal surface salinity perturbations influencing the meridional overturning circulation maximum are exhibited and interpreted on a stable steady state of a 2D latitude--depth ocean thermohaline circulation model. Despite the stability of the steady state, the nonnormality of the dynamics is able to create some transient growth and variability through stimulation by optimal perturbations. Two different measures are compared to obtain the optimum-one associated with the departure from steady state in terms of density, and the other with the overturning circulation intensity. It is found that such optimal analysis is measure dependent; hence, the latter measure is chosen for studying the following physical mechanisms. The response to the optimal initial sea surface salinity perturbation involves a transient growth mechanism leading to a maximum modification of the circulation intensity after 67 yr; the amplification is linked to the most weakly damped linear eigenmode, oscillating on a 150-yr period. Optimal constant surface salinity flux perturbations are also obtained, and confirm that a decrease in the freshwater flux amplitude enhances the circulation intensity. At last, looking for the optimal stochastic surface salinity flux perturbation, it is established that the variance of the circulation intensity is controlled by the weakly damped 150-yr oscillation. Two approaches are tested to consider extending such studies in more realistic 3D models. Explicit solutions (versus eigenvalue problems) are found for the overturning circulation measure (except for the stochastic optimal); a truncation method on a few leading eigenmodes usually provides the optimal perturbations for analyses on long time scales.}},2127 language = { Anglais},2128 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire de physique des oc{\'e}ans - LPO},2121 title = {{Optimal {S}urface {S}alinity {P}erturbations {I}nfluencing the {T}hermohaline {C}irculation.}}, 2122 author = {{F}lorian {S}évellec and {M}ahdi {B}en {J}elloul and {T}hierry {H}uck}, 2123 abstract = {{Optimal surface salinity perturbations influencing the meridional overturning circulation maximum are exhibited and interpreted on a stable steady state of a 2D latitude--depth ocean thermohaline circulation model. {D}espite the stability of the steady state, the nonnormality of the dynamics is able to create some transient growth and variability through stimulation by optimal perturbations. {T}wo different measures are compared to obtain the optimum-one associated with the departure from steady state in terms of density, and the other with the overturning circulation intensity. {I}t is found that such optimal analysis is measure dependent; hence, the latter measure is chosen for studying the following physical mechanisms. {T}he response to the optimal initial sea surface salinity perturbation involves a transient growth mechanism leading to a maximum modification of the circulation intensity after 67 yr; the amplification is linked to the most weakly damped linear eigenmode, oscillating on a 150-yr period. {O}ptimal constant surface salinity flux perturbations are also obtained, and confirm that a decrease in the freshwater flux amplitude enhances the circulation intensity. {A}t last, looking for the optimal stochastic surface salinity flux perturbation, it is established that the variance of the circulation intensity is controlled by the weakly damped 150-yr oscillation. {T}wo approaches are tested to consider extending such studies in more realistic 3D models. {E}xplicit solutions (versus eigenvalue problems) are found for the overturning circulation measure (except for the stochastic optimal); a truncation method on a few leading eigenmodes usually provides the optimal perturbations for analyses on long time scales.}}, 2124 language = {{A}nglais}, 2125 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire de physique des océans - LPO}, 2129 2126 pages = {2789-2808}, 2130 journal = { Journal of Physical Oceanography},2127 journal = {{J}ournal of {P}hysical {O}ceanography}, 2131 2128 volume = {37}, 2132 2129 number = {12}, … … 2142 2139 loceanaffectation = {ird}, 2143 2140 timestamp = {20121108}, 2144 title = {{Monitoramento das chuvas por sensoriamento remoto em Mato Grosso de 2000 a 2001}},2145 author = { Vincent Dubreuil and {J}osyane Ronchail and Gilda Maitelli},2146 language = { Portugais},2147 affiliation = { Littoral, Environnement, T{\'e}l{\'e}d{\'e}tection, G{\'e}omatique - LETG - Costel , Institut de recherche pour le d{\'e}veloppement - IRD , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Universidade Federal de Mato Grosso - UFMT},2148 booktitle = {{Anais do VI Simposio Brasileiro de Climatologia Geografica}},2149 pages = {8p. (CD- Rom)},2150 address = { Aracaju, Br{\'e}sil},2141 title = {{Monitoramento das chuvas por sensoriamento remoto em {M}ato {G}rosso de 2000 a 2001}}, 2142 author = {{V}incent {D}ubreuil and {J}osyane {R}onchail and {G}ilda {M}aitelli}, 2143 language = {{P}ortugais}, 2144 affiliation = {{L}ittoral, {E}nvironnement, {T}élédétection, {G}éomatique - LETG - {C}ostel , {I}nstitut de recherche pour le développement - IRD , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {U}niversidade {F}ederal de {M}ato {G}rosso - UFMT}, 2145 booktitle = {{Anais do VI {S}imposio {B}rasileiro de {C}limatologia {G}eografica}}, 2146 pages = {8p. (CD-{R}om)}, 2147 address = {{A}racaju, {B}résil}, 2151 2148 audience = {nationale}, 2152 2149 year = {2004}, … … 2158 2155 loceanaffectation = {ird}, 2159 2156 timestamp = {20121108}, 2160 title = {{Suivi de la saison des pluies 1999-2000 au Mato Grosso (Br{\'e}sil) par imagerie infrarouge GOES}},2161 author = { Vincent Dubreuil and Anne Jallet and Virginie Jumeau and {J}osyane Ronchail},2162 language = { Fran{\c c}ais},2163 affiliation = { Littoral, Environnement, T{\'e}l{\'e}d{\'e}tection, G{\'e}omatique - LETG - Costel , Institut de recherche pour le d{\'e}veloppement - IRD , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2164 booktitle = {{Actes du 16e Colloque de l'Association Internationale de Climatologie}},2157 title = {{Suivi de la saison des pluies 1999-2000 au {M}ato {G}rosso (Brésil) par imagerie infrarouge GOES}}, 2158 author = {{V}incent {D}ubreuil and {A}nne {J}allet and {V}irginie {J}umeau and {J}osyane {R}onchail}, 2159 language = {{F}rançais}, 2160 affiliation = {{L}ittoral, {E}nvironnement, {T}élédétection, {G}éomatique - LETG - {C}ostel , {I}nstitut de recherche pour le développement - IRD , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2161 booktitle = {{Actes du 16e {C}olloque de l'{A}ssociation {I}nternationale de {C}limatologie}}, 2165 2162 pages = {93-96}, 2166 address = { Varsovie, Pologne},2163 address = {{V}arsovie, {P}ologne}, 2167 2164 audience = {internationale}, 2168 2165 year = {2003}, … … 2175 2172 loceanteam = {varclim}, 2176 2173 timestamp = {20121108}, 2177 title = {{Potentialit {\'e}s des donn{\'e}es TRMM pour la spatialisation des pr{\'e}cipitations des pr{\'e}cipitations au Mato Grosso, Br{\'e}sil}},2178 author = { Vincent Dubreuil and {J}osyane {R}onchail and Damien Arvor},2179 abstract = {{The data provided by the algorithm 3B43 combining syntheses of microwaves images TRMM and ground data are, at the present time, one of the best product available to this space resolution for the rainfall cartography. For this study, these data were initially compared with the measurements made for 9 stations distributed on all Mato Grosso: the correlations between data TRMM and these stations vary from 0,84 (Pontes E Lacerda) to 0,94 (Xavantina) and show that TRMM data reproduce correctly the seasonal modes. TRMM Synthesis also allow to produce annual average maps of frequency of the dry months and a classification of the seasonal modes obtained after an analysis in principal components on the whole of the series.}},2180 keywords = { Pr{\'e}cipitations ; t{\'e}l{\'e}d{\'e}tection ; Amazonie ; ressource en eau},2181 language = { Fran{\c c}ais},2182 affiliation = { Littoral, Environnement, T{\'e}l{\'e}d{\'e}tection, G{\'e}omatique - LETG - Costel , Institut de recherche pour le d{\'e}veloppement - IRD , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2183 booktitle = {{Actes du XXe Colloque de l'Association Internationale de Climatologie}},2184 publisher = {AIC, Universit{\'e} de Tunis},2174 title = {{Potentialités des données TRMM pour la spatialisation des précipitations des précipitations au {M}ato {G}rosso, {B}résil}}, 2175 author = {{V}incent {D}ubreuil and {J}osyane {R}onchail and {D}amien {A}rvor}, 2176 abstract = {{The data provided by the algorithm 3B43 combining syntheses of microwaves images TRMM and ground data are, at the present time, one of the best product available to this space resolution for the rainfall cartography. {F}or this study, these data were initially compared with the measurements made for 9 stations distributed on all {M}ato {G}rosso: the correlations between data TRMM and these stations vary from 0,84 (Pontes E {L}acerda) to 0,94 (Xavantina) and show that TRMM data reproduce correctly the seasonal modes. TRMM {S}ynthesis also allow to produce annual average maps of frequency of the dry months and a classification of the seasonal modes obtained after an analysis in principal components on the whole of the series.}}, 2177 keywords = {{P}récipitations ; télédétection ; {A}mazonie ; ressource en eau}, 2178 language = {{F}rançais}, 2179 affiliation = {{L}ittoral, {E}nvironnement, {T}élédétection, {G}éomatique - LETG - {C}ostel , {I}nstitut de recherche pour le développement - IRD , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2180 booktitle = {{Actes du XXe {C}olloque de l'{A}ssociation {I}nternationale de {C}limatologie}}, 2181 publisher = {AIC, {U}niversité de {T}unis}, 2185 2182 pages = {210-215}, 2186 address = { Carthage, Tunisie},2187 editor = { H.Ben Boubaker},2183 address = {{C}arthage, {T}unisie}, 2184 editor = {{H}. Ben {B}oubaker}, 2188 2185 audience = {internationale}, 2189 2186 year = {2007}, … … 2197 2194 timestamp = {20121108}, 2198 2195 title = {{Implementation of an assimilative physical-biogeochemical coupled system}}, 2199 author = { P. Brasseur and D. Beal and J.M. Brankart and Y. Ourmières and A. El Moussaoui and {M}arina {L}évy and C. Moulin and P. Monfray},2200 language = { Anglais},2201 affiliation = { Laboratoire des {\'e}coulements g{\'e}ophysiques et industriels - LEGI , Laboratoire de sondages {\'e}lectromagn{\'e}tiques de l'environnement terrestre - LSEET , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire des sciences du climat et de l'environnement - LSCE},2196 author = {{P}. {B}rasseur and D. {B}eal and J.M. {B}rankart and Y. {O}urmières and A. {E}l {M}oussaoui and {M}arina {L}évy and C. {M}oulin and P. {M}onfray}, 2197 language = {{A}nglais}, 2198 affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {L}aboratoire de sondages électromagnétiques de l'environnement terrestre - LSEET , {L}aboratoire d'études en {G}éophysique et océanographie spatiales - LEGOS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire des sciences du climat et de l'environnement - LSCE}, 2202 2199 booktitle = {{4th MERSEA annual meeting}}, 2203 address = { Paris, France},2200 address = {{P}aris, {F}rance}, 2204 2201 year = {2008}, 2205 2202 } … … 2212 2209 timestamp = {20121108}, 2213 2210 title = {{Pros and cons of using seabirds as ecological indicators}}, 2214 author = {{J}oël {M}. {D}urant and D.O. and Hjermann and M. Frederiksen and {J}ean-{B}enoît {C}harrassin and {Y}von {{L}e {M}aho}and P. S. Sabarros and R.J.M. Crawford and N. Chr. Stenseth},2215 abstract = {{Climate change and overfishing are increasingly causing unanticipated changes in marine ecosystems (e.g. shifts in species dominance). In order to understand and anticipate these changes, there is a crucial need for indicators that summarise large quantities of information into a few relevant and accessible signals. Seabirds have been suggested as good candidates for ecological indicators of the marine environment; however, few studies have critically evaluated their value as such. We review the role of seabirds as ecological indicators, and discuss their limitations and drawbacks, as compared to other types of indicators. In addition, we highlight the statistical consequences of inverse inference when using seabird data as indicators. We discuss the use of integrated indices and the use of seabirds as autonomous samplers of the marine environment. Finally, we highlight the necessary steps preceding the use of seabirds as indicators. We conclude that, in order to use seabird time series properly, the use of recent advances both in statistics and in remote sensing is a way to move forward. This, along with the assessment of their usefulness, should enable us to use seabird indicators appropriately for managing urgent conservation problems.}},2216 keywords = { Food chain;Oceanography;Statistics;Conservation;Ecosystem-based management;Telemetry},2217 language = { Anglais},2218 affiliation = { Centre for Ecological and Evolutionary Synthesis - CEES , National Environmental Research Institute , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , D{\'e}partement Ecologie, Physiologie et Ethologie - DEPE-IPHC , Animal Demography Unit},2211 author = {{J}oël {M}. {D}urant and D.O. and {H}jermann and M. {F}rederiksen and {J}ean-{B}enoît {C}harrassin and {Y}von {{L}e {M}aho}and P. S. {S}abarros and R.J.M. {C}rawford and N. {C}hr. {S}tenseth}, 2212 abstract = {{Climate change and overfishing are increasingly causing unanticipated changes in marine ecosystems (e.g. shifts in species dominance). {I}n order to understand and anticipate these changes, there is a crucial need for indicators that summarise large quantities of information into a few relevant and accessible signals. {S}eabirds have been suggested as good candidates for ecological indicators of the marine environment; however, few studies have critically evaluated their value as such. {W}e review the role of seabirds as ecological indicators, and discuss their limitations and drawbacks, as compared to other types of indicators. {I}n addition, we highlight the statistical consequences of inverse inference when using seabird data as indicators. {W}e discuss the use of integrated indices and the use of seabirds as autonomous samplers of the marine environment. {F}inally, we highlight the necessary steps preceding the use of seabirds as indicators. {W}e conclude that, in order to use seabird time series properly, the use of recent advances both in statistics and in remote sensing is a way to move forward. {T}his, along with the assessment of their usefulness, should enable us to use seabird indicators appropriately for managing urgent conservation problems.}}, 2213 keywords = {{F}ood chain;Oceanography;Statistics;Conservation;Ecosystem-based management;Telemetry}, 2214 language = {{A}nglais}, 2215 affiliation = {{C}entre for {E}cological and {E}volutionary {S}ynthesis - CEES , {N}ational {E}nvironmental {R}esearch {I}nstitute , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {D}épartement {E}cologie, {P}hysiologie et {E}thologie - DEPE-IPHC , {A}nimal {D}emography {U}nit}, 2219 2216 pages = {115-129}, 2220 journal = { Climate Research},2217 journal = {{C}limate {R}esearch}, 2221 2218 volume = {39}, 2222 2219 audience = {internationale}, … … 2231 2228 loceanteam = {varclim}, 2232 2229 timestamp = {20121107}, 2233 title = {{Les a {\'e}rosols d{\'e}sertiques, un facteur potentiel des {\'e}pid{\'e}mies de m{\'e}ningite en Afrique de l'Ouest}},2230 title = {{Les aérosols désertiques, un facteur potentiel des épidémies de méningite en {A}frique de l'{O}uest}}, 2234 2231 author = {{N}adège {M}artiny and {I}sabelle {C}hiapello and {B}enjamin {S}ultan and {B}ernard {F}ontaine}, 2235 language = { Fran{\c c}ais},2236 affiliation = { Centre de Recherches de Climatologie - CRC , Laboratoire d'optique atmosph{\`e}rique - LOA , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2232 language = {{F}rançais}, 2233 affiliation = {{C}entre de {R}echerches de {C}limatologie - CRC , {L}aboratoire d'optique atmosphèrique - LOA , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2237 2234 pages = {VOL 10/3-4 - 2007 - pp.31-39}, 2238 journal = { Sant{\'e}-D{\'e}cision-Management},2235 journal = {{S}anté-{D}écision-{M}anagement}, 2239 2236 volume = {10}, 2240 2237 number = {3-4}, … … 2249 2246 loceanteam = {varclim}, 2250 2247 timestamp = {20121107}, 2251 title = {{Analysis of the relationships between climate/aerosols and meningitis epidemics in Western Africa}},2248 title = {{Analysis of the relationships between climate/aerosols and meningitis epidemics in {W}estern {A}frica}}, 2252 2249 author = {{N}adège {M}artiny and {I}sabelle {C}hiapello and {B}enjamin {S}ultan and {B}ernard {F}ontaine}, 2253 language = { Anglais},2254 affiliation = { Centre de Recherches de Climatologie - CRC , Laboratoire d'optique atmosph{\`e}rique - LOA , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2255 booktitle = {{Joint AMMA/ENSEMBLES Workshop}},2256 address = { Niamey, Niger},2250 language = {{A}nglais}, 2251 affiliation = {{C}entre de {R}echerches de {C}limatologie - CRC , {L}aboratoire d'optique atmosphèrique - LOA , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2252 booktitle = {{Joint AMMA/ENSEMBLES {W}orkshop}}, 2253 address = {{N}iamey, {N}iger}, 2257 2254 year = {2008}, 2258 2255 month = may, … … 2265 2262 loceanteam = {paleoproxus}, 2266 2263 timestamp = {20121107}, 2267 title = {{Linking Ocean Variabilty to Phytoplankton Changes Over the Last 2000 Years off N. Iceland}},2268 author = {{I}oanna {B}ouloubassi and {M}arie-{A}lexandrine {S}icre and Ullah Ezat and {G}eneviève {G}ondry and Jérémy Jacob and M. Azzoug},2269 abstract = {{Understanding ocean variability at decadal to century time-scale is a key issue of climate research, yet it remains poorly described partly because high resolution marine records are lacking. Recent observations also suggested that climate-driven oceanic changes may also affect marine productivity reflecting adjustments of the pelagic ecosystem. To explore these issues we investigated sediment cores (a Calypso and a box core) off North Iceland at unprecedented high temporal resolution (2 to 5 years). The area lies in a sensitive boundary region with strong climatic gradients between the Arctic and the North Atlantic realms. Surface hydrology is affected by warm, high salinity Atlantic water (Irminger current-IC) and cold, low salinity water of the East Icelandic Current (EIC), as well as by sea ice and drifting ice exported from the Arctic Ocean and East Greenland. Using biomarker proxies we reconstructed, over the past two millennia, high frequency surface ocean properties, such as Sea Surface Temperature (SST) and patterns of major phytoplankton groups. Records from a box core covering the last 80 years and comparison with instrumental data allowed to improve constrain of the proxies used. The SST curve reveals 4 major oscillations of about 20-25 years, depicting also the Great Salinity Anomaly (GSA). It reflects ocean circulation changes with varying impact of Polar and Atlantic waters (EIC, IC). Similarities with the NAO (North Atlantic Oscillation) index suggest links between STT and westerlies intensity. Phytoplankton biomarker profiles (specific phytosterols and alkenones) are consistent with biological data acquired during annual surveys. They show significant increase in periods when Atlantic waters and subsequent mixing processes prevail during positive NAO phase, compared to low levels when Polar waters and stratified conditions occur. Over the last two millennia the SST curve depicts a broad cooling trend towards present, steepening over the last 500 years. Prolonged warm or cool centennial intervals are recognizable among which the Medieval Warm Period (MWP), the Little Ice Age (LIA), the Roman Warm Period (RWP) and cooler Dark Ages. The SST signal also shows intermittent 20-25 year oscillations that are likely reflecting the ocean response to wind forcing, presumably the NAO. Phytoplankton biomarkers show important high frequency oscillations. Diatom sterols infer a broad decrease of siliceous productivity since 2000 yr BP with minimum values during the LIA, and a sharp rise after 200 yr BP. Such a trend is not observed for coccolithophorid biomarkers (alkenones), which show low centennial scale variations since 1200 yrs BP, along with high abundance between 1600 and 1200 yrs BP. Similar trends are observed for dinoflagellate biomarkers (dinosterol). Overall, planktonic biomarkers show multidecadal to centennial scale fluctuations inferring modifications of phytoplankton community structure. These could be linked at least partly to hydrological changes indicated in the SST curve, namely modifications of the relative importance of IC and EIC, which likely reflect the ocean response to NAO forcing.}},2270 language = { Anglais},2271 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire des sciences du climat et de l'environnement - LSCE , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO},2272 booktitle = {{EOS Trans AGU}},2264 title = {{Linking {O}cean {V}ariabilty to {P}hytoplankton {C}hanges {O}ver the {L}ast 2000 {Y}ears off N. {I}celand}}, 2265 author = {{I}oanna {B}ouloubassi and {M}arie-{A}lexandrine {S}icre and {U}llah {E}zat and {G}eneviève {G}ondry and {J}érémy {J}acob and M. {A}zzoug}, 2266 abstract = {{Understanding ocean variability at decadal to century time-scale is a key issue of climate research, yet it remains poorly described partly because high resolution marine records are lacking. {R}ecent observations also suggested that climate-driven oceanic changes may also affect marine productivity reflecting adjustments of the pelagic ecosystem. {T}o explore these issues we investigated sediment cores (a {C}alypso and a box core) off {N}orth {I}celand at unprecedented high temporal resolution (2 to 5 years). {T}he area lies in a sensitive boundary region with strong climatic gradients between the {A}rctic and the {N}orth {A}tlantic realms. {S}urface hydrology is affected by warm, high salinity {A}tlantic water (Irminger current-IC) and cold, low salinity water of the {E}ast {I}celandic {C}urrent (EIC), as well as by sea ice and drifting ice exported from the {A}rctic {O}cean and {E}ast {G}reenland. {U}sing biomarker proxies we reconstructed, over the past two millennia, high frequency surface ocean properties, such as {S}ea {S}urface {T}emperature (SST) and patterns of major phytoplankton groups. {R}ecords from a box core covering the last 80 years and comparison with instrumental data allowed to improve constrain of the proxies used. {T}he SST curve reveals 4 major oscillations of about 20-25 years, depicting also the {G}reat {S}alinity {A}nomaly (GSA). {I}t reflects ocean circulation changes with varying impact of {P}olar and {A}tlantic waters (EIC, IC). {S}imilarities with the NAO (North {A}tlantic {O}scillation) index suggest links between STT and westerlies intensity. {P}hytoplankton biomarker profiles (specific phytosterols and alkenones) are consistent with biological data acquired during annual surveys. {T}hey show significant increase in periods when {A}tlantic waters and subsequent mixing processes prevail during positive NAO phase, compared to low levels when {P}olar waters and stratified conditions occur. {O}ver the last two millennia the SST curve depicts a broad cooling trend towards present, steepening over the last 500 years. {P}rolonged warm or cool centennial intervals are recognizable among which the {M}edieval {W}arm {P}eriod (MWP), the {L}ittle {I}ce {A}ge (LIA), the {R}oman {W}arm {P}eriod (RWP) and cooler {D}ark {A}ges. {T}he SST signal also shows intermittent 20-25 year oscillations that are likely reflecting the ocean response to wind forcing, presumably the NAO. {P}hytoplankton biomarkers show important high frequency oscillations. {D}iatom sterols infer a broad decrease of siliceous productivity since 2000 yr BP with minimum values during the LIA, and a sharp rise after 200 yr BP. {S}uch a trend is not observed for coccolithophorid biomarkers (alkenones), which show low centennial scale variations since 1200 yrs BP, along with high abundance between 1600 and 1200 yrs BP. {S}imilar trends are observed for dinoflagellate biomarkers (dinosterol). {O}verall, planktonic biomarkers show multidecadal to centennial scale fluctuations inferring modifications of phytoplankton community structure. {T}hese could be linked at least partly to hydrological changes indicated in the SST curve, namely modifications of the relative importance of IC and EIC, which likely reflect the ocean response to NAO forcing.}}, 2267 language = {{A}nglais}, 2268 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire des sciences du climat et de l'environnement - LSCE , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO}, 2269 booktitle = {{EOS {T}rans AGU}}, 2273 2270 publisher = {AGU}, 2274 2271 pages = {51B-1494}, 2275 address = { France},2272 address = {{F}rance}, 2276 2273 volume = {89}, 2277 2274 number = {53}, … … 2286 2283 loceanteam = {paleoproxus}, 2287 2284 timestamp = {20121107}, 2288 title = { Changements r{\'e}cents de l'environnement et des activit{\'e}s humaines autour du Lac du Boqueir{\\~a}o (Nord Est Br{\'e}sil)},2285 title = {{C}hangements récents de l'environnement et des activités humaines autour du {L}ac du {B}oqueirão (Nord {E}st {B}résil)}, 2289 2286 author = {{R}enata {Z}ocatelli and {B}runo {T}urcq and {J}érémy {J}acob and {M}ohammed {B}oussafir and {J}ean-{R}obert {D}isnar and {A}bdelfettah {S}ifeddine}, 2290 language = { Fran{\c c}ais},2291 affiliation = { Departamento de Geoqu{\'\i}mica , Pal{\'e}o-environnements tropicaux et variabilit{\'e} climatique - PALEOTROPIQUE , Departamento de Geoquimica - DEPARTAMENTO DE GEOQUIMICA , Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2292 booktitle = {{Mati {\`e}res Organiques et Environnement}},2287 language = {{F}rançais}, 2288 affiliation = {{D}epartamento de {G}eoquìmica , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA , {I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2289 booktitle = {{Matières {O}rganiques et {E}nvironnement}}, 2293 2290 pages = {1 p.}, 2294 address = { France},2291 address = {{F}rance}, 2295 2292 audience = {nationale}, 2296 2293 year = {2009}, … … 2301 2298 loceanbibid = {01779}, 2302 2299 timestamp = {20121107}, 2303 title = {{Rapid paleoenvironmental variations in NE Brazil during the Lateglacial. Insights from TpS2, S3CO2 and S3CO Rock Eval parameters.}},2304 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir Didier Kéravis and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq},2305 abstract = {{The Rock-Eval pyrolysis technique was first developed as a rapid mean for evaluating the petroleum potential of source rocks, via the measurement of bulk organic parameters such as Total Organic Carbon (TOC), Hydrogen Index (HI), Oxygen Index (OI) and the maximum pyrolysis temperature Tmax (Espitali{\'e} et al., 1985; Lafargue et al., 1998). This method was then used to rapidly estimate organic matter quality and quantity in sedimentary series for paleoenvironmental studies (Talbot and Livingston, 1989). Recently, it has been proposed that there could be more information gained from the Rock-Eval parameters (Disnar et al., 2003). When considering also the recent analytical developments available from the Turbo6 version of the apparatus, there is a large field of investigation that remains unexplored in paleoenvironmental studies. Here we present results from the sedimentary infill of Lagoa do Ca{\c c}{\'o} (Northern Brazil) that records paleoenvironmental changes since the Last Glacial Maximum (Jacob et al., 2004). The present study focuses on the Lateglacial interval (ca. 17,000 to 11,000 cal yrs BP), a time period where different Rock-Eval parameters such as TpS2 (Tmax equivalent), HI and OI produce controversial information. In order to better understand the meaning of these parameters, we propose an original mean of obtaining more pertinent information. S3CO2/S3CO ratio and TpS2 surprisingly display similar trends over the considered period, in two different cores. Furthermore, the evolution of these parameters is comparable with that of #18O in the ice core record of Sajama (Bolivia) during the Lateglacial (Figure 1). Although the significance of these parameters and the origin of these variations remain to be cleared, our results confirm a pattern of rapid climate variability over the South American Tropics during the last deglaciation, as seen in the Northern Hemisphere.}},2306 language = { Anglais},2307 affiliation = { Institut des Sciences de la Terre d'Orl{\'e}ans - ISTO , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Departamento de Geoquimica - DEPARTAMENTO DE GEOQUIMICA , Pal{\'e}o-environnements tropicaux et variabilit{\'e}climatique - PALEOTROPIQUE},2300 title = {{Rapid paleoenvironmental variations in NE {B}razil during the {L}ateglacial. {I}nsights from {T}pS2, S3CO2 and S3CO {R}ock {E}val parameters.}}, 2301 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir {D}idier {K}éravis and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 2302 abstract = {{The {R}ock-{E}val pyrolysis technique was first developed as a rapid mean for evaluating the petroleum potential of source rocks, via the measurement of bulk organic parameters such as {T}otal {O}rganic {C}arbon (TOC), {H}ydrogen {I}ndex (HI), {O}xygen {I}ndex (OI) and the maximum pyrolysis temperature {T}max (Espitalié et al., 1985; {L}afargue et al., 1998). {T}his method was then used to rapidly estimate organic matter quality and quantity in sedimentary series for paleoenvironmental studies (Talbot and {L}ivingston, 1989). {R}ecently, it has been proposed that there could be more information gained from the {R}ock-{E}val parameters (Disnar et al., 2003). {W}hen considering also the recent analytical developments available from the {T}urbo6 version of the apparatus, there is a large field of investigation that remains unexplored in paleoenvironmental studies. {H}ere we present results from the sedimentary infill of {L}agoa do {C}açó (Northern {B}razil) that records paleoenvironmental changes since the {L}ast {G}lacial {M}aximum (Jacob et al., 2004). {T}he present study focuses on the {L}ateglacial interval (ca. 17,000 to 11,000 cal yrs BP), a time period where different {R}ock-{E}val parameters such as {T}pS2 (Tmax equivalent), HI and OI produce controversial information. {I}n order to better understand the meaning of these parameters, we propose an original mean of obtaining more pertinent information. S3CO2/S3CO ratio and {T}pS2 surprisingly display similar trends over the considered period, in two different cores. {F}urthermore, the evolution of these parameters is comparable with that of #18O in the ice core record of {S}ajama (Bolivia) during the {L}ateglacial (Figure 1). {A}lthough the significance of these parameters and the origin of these variations remain to be cleared, our results confirm a pattern of rapid climate variability over the {S}outh {A}merican {T}ropics during the last deglaciation, as seen in the {N}orthern {H}emisphere.}}, 2303 language = {{A}nglais}, 2304 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 2308 2305 booktitle = {{IMOG meeting}}, 2309 2306 pages = {2 p.}, 2310 address = { S{\'e}ville, Espagne},2307 address = {{S}éville, {E}spagne}, 2311 2308 editor = {IMOG}, 2312 2309 audience = {internationale}, … … 2320 2317 loceanteam = {surf}, 2321 2318 timestamp = {20121107}, 2322 title = { Interpretation of CAROLS L-Band measurements in the Gulf of Biscaye},2323 author = {{A}drien {M}artin and {J}acqueline {B}outin and Danièle Hauser and {G}illes {R}everdin and {M}ickael {P}ardé and {M}ehrez {Z}ribi and {P}. {F}anise and {J}. {T}enerelli and {N}. {R}eul},2324 abstract = {{The L-band Cooperative Airborne Radiometer for Ocean and Land Studies (CAROLS) radiometer (Zribi et al., IGARSS 2008) flew seven times over the Gulf of Biscay between May 04 and May 26, 2009 around 20UTC. These flights followed two airborne campaigns with the same instrument in September 2007 and November 2008. Brightness temperatures (Tb) of the surface were measured by one antenna looking at 33° on the right hand side of the aircraft and optionally by a nadir antenna. The nadir antenna is sometimes exchanged with the radar scatterometer STORM in order to get a measurement of surface roughness, related to wind, coincident in space and time with the radiometric measurement. Measurements are compared with simulations conducted with the Terrestrial Radiometry Analysis Package (TRAP) (Tenerelli et al., 2008) software run for CAROLS geometry and different observed geophysical conditions. Concomitant ship campaign and drifter deployments provide in situ ground truths for sea surface salinity and temperature. Wind speed and direction are either estimated from the QSCAT scatterometer or from the STORM scatterometer and complemented with in situ observation TRAP uses the physical modeling of atmospheric radiative transfer, sea surface emissivity and galactic glint foreseen for the processing of the Soil Moisture and Ocean Salinity satellite data. The circle flights and wing-wags movements of the CAROLS aircraft (The French research ATR42 aircraft) allow to explore a wide range of incidence angles (from 0° to about 60°) and of galactic signals reflected by the sea surface. Previous flights in 2008 and 2009 have demonstrated that on a whole, simulated and observed variations of Tb with incidence angle are very consistent, demonstrating a good sensitivity of CAROLS instrument. In this presentation we will focus on the correlation between L-band radiometer measurements and scatterometer measurements, especially in a case of strong spatial gradient of wind speed (1 to 10m/s) observed in 2007 and on the signature of coastal salinity gradients on the L-band radiometer observed in 2009 during which we observed SSS variations between roughly 32 and 35.6 pss. New CAROLS flights in the Gulf of Biscay are foreseen in April and May 2010 under the track of the SMOS satellite.}},2325 language = { Anglais},2326 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Institut Pierre-Simon-Laplace - IPSL , Centre d'{\'e}tudes spatiales de la biosph{\`e}re - CESBIO , CLS Brest , Institut Fran{\c c}ais de Recherche et d'Exploitation de la Mer - IFREMER},2327 booktitle = {{ESA Living Planet Symposium, ESA-SP 686}},2328 address = { Bergen, Norv{\`e}ge},2319 title = {{I}nterpretation of CAROLS L-{B}and measurements in the {G}ulf of {B}iscaye}, 2320 author = {{A}drien {M}artin and {J}acqueline {B}outin and {D}anièle {H}auser and {G}illes {R}everdin and {M}ickael {P}ardé and {M}ehrez {Z}ribi and {P}. {F}anise and {J}. {T}enerelli and {N}. {R}eul}, 2321 abstract = {{The L-band {C}ooperative {A}irborne {R}adiometer for {O}cean and {L}and {S}tudies (CAROLS) radiometer (Zribi et al., IGARSS 2008) flew seven times over the {G}ulf of {B}iscay between {M}ay 04 and {M}ay 26, 2009 around 20UTC. {T}hese flights followed two airborne campaigns with the same instrument in {S}eptember 2007 and {N}ovember 2008. {B}rightness temperatures (Tb) of the surface were measured by one antenna looking at 33° on the right hand side of the aircraft and optionally by a nadir antenna. {T}he nadir antenna is sometimes exchanged with the radar scatterometer STORM in order to get a measurement of surface roughness, related to wind, coincident in space and time with the radiometric measurement. {M}easurements are compared with simulations conducted with the {T}errestrial {R}adiometry {A}nalysis {P}ackage (TRAP) (Tenerelli et al., 2008) software run for CAROLS geometry and different observed geophysical conditions. {C}oncomitant ship campaign and drifter deployments provide in situ ground truths for sea surface salinity and temperature. {W}ind speed and direction are either estimated from the QSCAT scatterometer or from the STORM scatterometer and complemented with in situ observation TRAP uses the physical modeling of atmospheric radiative transfer, sea surface emissivity and galactic glint foreseen for the processing of the {S}oil {M}oisture and {O}cean {S}alinity satellite data. {T}he circle flights and wing-wags movements of the CAROLS aircraft (The {F}rench research ATR42 aircraft) allow to explore a wide range of incidence angles (from 0° to about 60°) and of galactic signals reflected by the sea surface. {P}revious flights in 2008 and 2009 have demonstrated that on a whole, simulated and observed variations of {T}b with incidence angle are very consistent, demonstrating a good sensitivity of CAROLS instrument. {I}n this presentation we will focus on the correlation between L-band radiometer measurements and scatterometer measurements, especially in a case of strong spatial gradient of wind speed (1 to 10m/s) observed in 2007 and on the signature of coastal salinity gradients on the L-band radiometer observed in 2009 during which we observed SSS variations between roughly 32 and 35.6 pss. {N}ew CAROLS flights in the {G}ulf of {B}iscay are foreseen in {A}pril and {M}ay 2010 under the track of the SMOS satellite.}}, 2322 language = {{A}nglais}, 2323 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {C}entre d'études spatiales de la biosphère - CESBIO , CLS {B}rest , {I}nstitut {F}rançais de {R}echerche et d'{E}xploitation de la {M}er - IFREMER}, 2324 booktitle = {{ESA {L}iving {P}lanet {S}ymposium, ESA-SP 686}}, 2325 address = {{B}ergen, {N}orvège}, 2329 2326 audience = {internationale}, 2330 2327 year = {2010}, … … 2336 2333 loceanbibid = {01777}, 2337 2334 timestamp = {20121107}, 2338 title = {{Evidence of a shift in the cyclicity of Antarctic seabird dynamics linked to climate.}},2339 author = { St{\'e}phanie Jenouvrier and Henri Weimerskirch and Christophe Barbraud and {Y}oung-{H}yang {P}ark and Bernard Cazelles},2340 abstract = {{Ecosystems and populations are known to be influenced not only by long-term climatic trends, but also by other short-term climatic modes, such as interannual and decadal-scale variabilities. Because interactions between climatic forcing, biotic and abiotic components of ecosystems are subtle and complex, analysis of long-term series of both biological and physical factors is essential to understanding these interactions. Here, we apply a wavelet analysis simultaneously to long-term datasets on the environment and on the populations and breeding success of three Antarctic seabirds (southern fulmar, snow petrel, emperor penguin) breeding in Terre Ad{\'e}lie, to study the effects of climate fluctuations on Antarctic marine ecosystems. We show that over the past 40 years, populations and demographic parameters of the three species fluctuate with a periodicity of 3-5 years that was also detected in sea-ice extent and the Southern Oscillation Index. Although the major periodicity of these interannual fluctuations is not common to different species and environmental variables, their cyclic characteristics reveal a significant change since 1980. Moreover, sliding-correlation analysis highlighted the relationships between environmental variables and the demography of the three species, with important change of correlation occurring between the end of the 1970s and the beginning of the 1980s. These results suggest that a regime shift has probably occurred during this period, significantly affecting the Antarctic ecosystem, but with contrasted effects on the three species.}},2341 language = { Anglais},2342 affiliation = { Centre d'{\'e}tudes biologiques de Chiz{\'e} - CEBC , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Fonctionnement et {\'e}volution des syst{\`e}mes {\'e}cologiques - FESE , Mod{\'e}lisation math{\'e}matique et informatique de syst{\`e}mes complexes naturels, biologiques ou sociaux - GEODES},2335 title = {{Evidence of a shift in the cyclicity of {A}ntarctic seabird dynamics linked to climate.}}, 2336 author = {{S}téphanie {J}enouvrier and {H}enri {W}eimerskirch and {C}hristophe {B}arbraud and {Y}oung-{H}yang {P}ark and {B}ernard {C}azelles}, 2337 abstract = {{Ecosystems and populations are known to be influenced not only by long-term climatic trends, but also by other short-term climatic modes, such as interannual and decadal-scale variabilities. {B}ecause interactions between climatic forcing, biotic and abiotic components of ecosystems are subtle and complex, analysis of long-term series of both biological and physical factors is essential to understanding these interactions. {H}ere, we apply a wavelet analysis simultaneously to long-term datasets on the environment and on the populations and breeding success of three {A}ntarctic seabirds (southern fulmar, snow petrel, emperor penguin) breeding in {T}erre {A}délie, to study the effects of climate fluctuations on {A}ntarctic marine ecosystems. {W}e show that over the past 40 years, populations and demographic parameters of the three species fluctuate with a periodicity of 3-5 years that was also detected in sea-ice extent and the {S}outhern {O}scillation {I}ndex. {A}lthough the major periodicity of these interannual fluctuations is not common to different species and environmental variables, their cyclic characteristics reveal a significant change since 1980. {M}oreover, sliding-correlation analysis highlighted the relationships between environmental variables and the demography of the three species, with important change of correlation occurring between the end of the 1970s and the beginning of the 1980s. {T}hese results suggest that a regime shift has probably occurred during this period, significantly affecting the {A}ntarctic ecosystem, but with contrasted effects on the three species.}}, 2338 language = {{A}nglais}, 2339 affiliation = {{C}entre d'études biologiques de {C}hizé - CEBC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {F}onctionnement et évolution des systèmes écologiques - FESE , {M}odélisation mathématique et informatique de systèmes complexes naturels, biologiques ou sociaux - GEODES}, 2343 2340 pages = {887-895}, 2344 journal = { Proceedings of the Royal Society of London Series B Biological Sciences},2341 journal = {{P}roceedings of the {R}oyal {S}ociety of {L}ondon {S}eries B {B}iological {S}ciences}, 2345 2342 volume = {272}, 2346 2343 number = {1566}, … … 2358 2355 loceanteam = {paleoproxus}, 2359 2356 timestamp = {20121107}, 2360 title = {{Hydrologie et g {\'e}ochimie de lacs de Maars du sud-ouest Tanzanien et d'ailleurs : interactions entre eaux de surface, souterraines et hydrothermales}},2361 author = {{L}aurent {B}ergonzini and {M}anuëlla {D}elalande and P. Branchu and M. Massault and J.-C. Parisot and A. Majule and {D}avid {W}illiamson},2362 language = { Anglais},2363 affiliation = {IDES - Universit{\'e} Paris-Sud XI , Centre europ{\'e}en de recherche et d'enseignement de g{\'e}osciences de l'environnement - CEREGE , LOCEAN},2357 title = {{Hydrologie et géochimie de lacs de {M}aars du sud-ouest {T}anzanien et d'ailleurs : interactions entre eaux de surface, souterraines et hydrothermales}}, 2358 author = {{L}aurent {B}ergonzini and {M}anuëlla {D}elalande and P. {B}ranchu and M. {M}assault and J.-{C}. {P}arisot and A. {M}ajule and {D}avid {W}illiamson}, 2359 language = {{A}nglais}, 2360 affiliation = {IDES - {U}niversité {P}aris-{S}ud XI , {C}entre européen de recherche et d'enseignement de géosciences de l'environnement - CEREGE , LOCEAN}, 2364 2361 booktitle = {{RST}}, 2365 address = { Bordeaux, France},2362 address = {{B}ordeaux, {F}rance}, 2366 2363 year = {2010}, 2367 2364 month = oct, … … 2374 2371 loceanteam = {paleoproxus}, 2375 2372 timestamp = {20121107}, 2376 title = { Fluid geochemistry of natural manifestations from the Southern Poroto-Rungwe hydrothermal system (Tanzania) : preliminary conceptual model},2377 language = { Anglais},2373 title = {{F}luid geochemistry of natural manifestations from the {S}outhern {P}oroto-{R}ungwe hydrothermal system (Tanzania) : preliminary conceptual model}, 2374 language = {{A}nglais}, 2378 2375 author = {{M}anuëlla {D}elalande and {L}aurent {B}ergonzini and {F}abrizio {G}herardi and {M}assimo {G}uidi and {L}uc {A}ndre and {I}ssah {A}bdallah and {D}avid {W}illiamson}, 2379 affiliation = {IDES - Universit{\'e} Paris-Sud XI , UNIVERSITY OF FIRENZE Dipt di Biologia Animale e Genetica "Leo Pardi" - UNIVERSITY OF FIRENZE , CNR Institute of Geoscience and Earth Resources , Section de P{\'e}trographie-Min{\'e}ralogie-G{\'e}ochimie , IRA Institute of Resource Assessment , LOCEAN},2376 affiliation = {IDES - {U}niversité {P}aris-{S}ud XI , UNIVERSITY OF FIRENZE {D}ipt di {B}iologia {A}nimale e {G}enetica "Leo {P}ardi" - UNIVERSITY OF FIRENZE , CNR {I}nstitute of {G}eoscience and {E}arth {R}esources , {S}ection de {P}étrographie-{M}inéralogie-{G}éochimie , IRA {I}nstitute of {R}esource {A}ssessment , LOCEAN}, 2380 2377 booktitle = {{RST}}, 2381 address = { Bordeaux, France},2378 address = {{B}ordeaux, {F}rance}, 2382 2379 year = {2010}, 2383 2380 month = oct, … … 2390 2387 loceanteam = {paleoproxus}, 2391 2388 timestamp = {20121107}, 2392 title = {{Chronologie des monuments fun {\'e}raires sahariens : probl{\`e}mes, m{\'e}thode et r{\'e}sultats}},2393 author = { Françoise Paris and {J}ean-{F}rançois {S}aliège},2394 keywords = { Niger ; Afrique de l'Ouest ; Sahara central ; Pr{\'e}histoire ; Protohistoire ; s{\'e}pulture ; AMS ; datation ; radiocarbone ; m{\'e}thodologie ; ossements humains ;},2395 language = { Fran{\c c}ais},2396 affiliation = { Laboratoire m{\'e}diterran{\'e}en de pr{\'e}histoire Europe-Afrique - LAMPEA , Dynamique soci{\'e}t{\'e}s-environnements sur le temps long en Afrique p{\'e}risaharienne , LOCEAN},2389 title = {{Chronologie des monuments funéraires sahariens : problèmes, méthode et résultats}}, 2390 author = {{F}rançoise {P}aris and {J}ean-{F}rançois {S}aliège}, 2391 keywords = {{N}iger ; {A}frique de l'{O}uest ; {S}ahara central ; {P}réhistoire ; {P}rotohistoire ; sépulture ; AMS ; datation ; radiocarbone ; méthodologie ; ossements humains ;}, 2392 language = {{F}rançais}, 2393 affiliation = {{L}aboratoire méditerranéen de préhistoire {E}urope-{A}frique - LAMPEA , {D}ynamique sociétés-environnements sur le temps long en {A}frique périsaharienne , LOCEAN}, 2397 2394 pages = {57-60}, 2398 journal = { Nouvelles de l'Arch{\'e}ologie},2399 volume = {120-121 "Dossier : La coop{\'e}ration arch{\'e}ologique fran{\c c}aise en Afrique. 1 : Pr{\'e}histoire et protohistoi},2395 journal = {{N}ouvelles de l'{A}rchéologie}, 2396 volume = {120-121 "Dossier : {L}a coopération archéologique française en {A}frique. 1 : {P}réhistoire et protohistoi}, 2400 2397 audience = {nationale}, 2401 2398 year = {2010}, … … 2408 2405 loceanteam = {nemo,varclim,phybiocar}, 2409 2406 timestamp = {20121107}, 2410 title = { The regional coupled system WRF-NEMO over the Mediterranean (MORCE platform): impacts of mesoscale coupled processes on the water budget estimation},2407 title = {{T}he regional coupled system WRF-NEMO over the {M}editerranean (MORCE platform): impacts of mesoscale coupled processes on the water budget estimation}, 2411 2408 author = {{C}indy {L}ebeaupin-{B}rossier and {K}arine {B}éranger and {P}hilippe {D}robinski and {S}ophie {B}astin and {S}ylvain {M}ailler and {G}uillaume {S}amson and {S}ébastien {M}asson and {G}urvan {M}adec and {S}ophie {V}alcke and {L}aure {C}oquart and {E}ric {M}aisonnave}, 2412 language = { Anglais},2413 affiliation = { Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD , {\'E}cole Nationale Sup{\'e}rieure de Techniques Avanc{\'e}es - ENSTA ParisTech , Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , {\'E}cole Nationale des Ponts et Chauss{\'e}es , Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Centre Europ{\'e}en de Recherche et de Formation Avanc{\'e}e en Calcul Scientifique - CERFACS},2414 booktitle = {{5th HYMEX (HYdrological cycle Mediterranean EXperiment) Workshop}},2415 address = { Menorca, Espagne},2416 audience = {non sp {\'e}cifi{\'e}e},2409 language = {{A}nglais}, 2410 affiliation = {{L}aboratoire de {M}étéorologie {D}ynamique - LMD , École {N}ationale {S}upérieure de {T}echniques {A}vancées - ENSTA {P}arisTech , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , École {N}ationale des {P}onts et {C}haussées , {G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {C}entre {E}uropéen de {R}echerche et de {F}ormation {A}vancée en {C}alcul {S}cientifique - CERFACS}, 2411 booktitle = {{5th HYMEX (HYdrological cycle {M}editerranean EXperiment) {W}orkshop}}, 2412 address = {{M}enorca, {E}spagne}, 2413 audience = {non spécifiée}, 2417 2414 year = {2011}, 2418 2415 } … … 2424 2421 loceanbibid = {01772}, 2425 2422 timestamp = {20121107}, 2426 title = {{The role of synoptic scale dryair intrusions on the West African monsoon onset using regional modeling and nudged climate simulations. Application to the monsoon onset of 2006}},2423 title = {{The role of synoptic scale dryair intrusions on the {W}est {A}frican monsoon onset using regional modeling and nudged climate simulations. {A}pplication to the monsoon onset of 2006}}, 2427 2424 author = {{S}erge {J}anicot and {E}mmanouil {F}laounas and {S}ophie {B}astin and {R}émy {R}oca and {E}lsa {M}ohino}, 2428 language = { Anglais},2429 affiliation = { Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD},2430 booktitle = {{World Climate Research Programme (WCRP) Open Science Conference}},2425 language = {{A}nglais}, 2426 affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire de {M}étéorologie {D}ynamique - LMD}, 2427 booktitle = {{World {C}limate {R}esearch {P}rogramme (WCRP) {O}pen {S}cience {C}onference}}, 2431 2428 pages = {15 p.}, 2432 address = { Denver, {\'E}tats-Unis},2433 audience = {non sp {\'e}cifi{\'e}e},2429 address = {{D}enver, États-{U}nis}, 2430 audience = {non spécifiée}, 2434 2431 year = {2011}, 2435 2432 } … … 2441 2438 loceanbibid = {01771}, 2442 2439 timestamp = {20121107}, 2443 title = {{HyMeX - Model of the Regional Coupled Earth system (MORCE): application to process and climate studies in the Mediterranean region. (poster)}},2440 title = {{HyMeX - {M}odel of the {R}egional {C}oupled {E}arth system (MORCE): application to process and climate studies in the {M}editerranean region. (poster)}}, 2444 2441 author = {{Ph}ilippe {D}robinski and {A}lessandro {A}nav and {C}yndy {L}ebeaupin-{B}rossier and {G}uillaume {S}amson and {M}arc {S}tefanon and {S}ophie {B}astin and {M}élika {B}aklouti and {K}arine {B}eranger and {J}onathan {B}euvier and {R}omain {B}ourdalle-{B}adief and {L}aure {C}oquart and {F}abio D'{A}ndrea and {N}athalie de {N}oblet and {F}rédéric {D}iaz and {J}ean-{C}laude {D}utay and {Ch}ristian {É}thé and {M}arie-{A}lice {F}oujols and {D}mitry {K}hvorostiyanov and {G}urvan {M}adec and Éric {M}aisonnave and {M}artial {M}ancip and {S}ébastien {M}asson and {L}aurent {M}enut and {J}ulien {P}almieri and {J}an {P}olcher and {S}ophie {V}alcke and {N}icolas {V}iovy}, 2445 language = { Anglais},2446 affiliation = { Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD , Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME , Laboratoire de l'Atmosph{\`e}re et des Cyclones - LACy , Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire d'Oc{\'e}anographie Physique et Biog{\'e}ochimique - LOPB , {\'E}cole Nationale Sup{\'e}rieure de Techniques Avanc{\'e}es - ENSTA ParisTech , Unit{\'e} de M{\'e}canique - UME , Laboratoire d'informatique pour la mecanique et les sciences de l'ingenieur , Laboratoire Charles Fabry de l'Institut d'Optique - LCFIO , Laboratoire d'oc{\'e}anographie dynamique et de climatologie - LODYC , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Centre Europ{\'e}en de Recherche et de Formation Avanc{\'e}e en Calcul Scientifique - CERFACS , Frontier Research Center for Global Change , Laboratoire des sciences du climat et de l'environnement - LSCE},2447 booktitle = {{WCRP Open Science Conference}},2448 address = { Denver, {\'E}tats-Unis},2449 audience = {non sp {\'e}cifi{\'e}e},2442 language = {{A}nglais}, 2443 affiliation = {{L}aboratoire de {M}étéorologie {D}ynamique - LMD , {G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME , {L}aboratoire de l'{A}tmosphère et des {C}yclones - LACy , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire d'{O}céanographie {P}hysique et {B}iogéochimique - LOPB , École {N}ationale {S}upérieure de {T}echniques {A}vancées - ENSTA {P}arisTech , {U}nité de {M}écanique - UME , {L}aboratoire d'informatique pour la mecanique et les sciences de l'ingenieur , {L}aboratoire {C}harles {F}abry de l'{I}nstitut d'{O}ptique - LCFIO , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {C}entre {E}uropéen de {R}echerche et de {F}ormation {A}vancée en {C}alcul {S}cientifique - CERFACS , {F}rontier {R}esearch {C}enter for {G}lobal {C}hange , {L}aboratoire des sciences du climat et de l'environnement - LSCE}, 2444 booktitle = {{WCRP {O}pen {S}cience {C}onference}}, 2445 address = {{D}enver, États-{U}nis}, 2446 audience = {non spécifiée}, 2450 2447 year = {2011}, 2451 2448 month = oct, … … 2458 2455 loceanbibid = {01770}, 2459 2456 timestamp = {20121107}, 2460 title = {{Evaluation of the impact of albedo, orography, SST and large scale conditions on the 2006 West African Monsoon onset}},2457 title = {{Evaluation of the impact of albedo, orography, SST and large scale conditions on the 2006 {W}est {A}frican {M}onsoon onset}}, 2461 2458 author = {{E}mmanouil {F}laounas and {S}ophie {B}astin and {S}erge {J}anicot}, 2462 language = { Anglais},2463 affiliation = { Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2464 booktitle = {{3rd International AMMA Conference}},2465 address = { Ouagadougou, Burkina Faso},2466 audience = {non sp {\'e}cifi{\'e}e},2459 language = {{A}nglais}, 2460 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2461 booktitle = {{3rd {I}nternational AMMA {C}onference}}, 2462 address = {{O}uagadougou, {B}urkina {F}aso}, 2463 audience = {non spécifiée}, 2467 2464 year = {2009}, 2468 2465 } … … 2474 2471 loceanbibid = {01769}, 2475 2472 timestamp = {20121107}, 2476 title = {{SMOS First Results Successes and Issues: Towards Global Soil Moisture and Sea Sea Salinity Maps}},2477 author = {{Y}ann {H}. {K}err and {Ph}ilippe {W}aldteufel and {F}. {C}abot and P. Richaume and A. Mahmoodi and Steven Delwart and {J}ean-{P}ierre {W}igneron and {S}. {M}ecklenburg and {N}icolas {R}eul and {J}acqueline {B}outin},2478 abstract = {{SMOS, a L Band radiometer using aperture synthesis to achieve a good spatial resolution, was successfully launched on November 2, 2009. It was developed and made under the leadership of the European Space Agency (ESA) as an Earth Explorer Opportunity mission. It is a joint program with the Centre National d'Etudes Spatiales (CNES) in France and the Centro para el Desarrollo Teccnologico Industrial (CDTI) in Spain. SMOS carries a single payload, an L band 2D interferometric, radiometer in the 1400-1427 MHz h protected band. This wavelength penetrates well through the vegetation and the atmosphere is almost transparent enabling to infer both soil moisture and vegetation water content over land and sea surface salinity over the oceans. SMOS achieves an unprecedented spatial resolution of 50 km at L-band maximum (43 km on average) with multi angular-dual polarized (or fully polarized) brightness temperatures over the globe and with a revisit time smaller than 3 days. SMOS as been now acquiring data for over one year after the end of the commissioning phase. The data quality exceeds what was expected, showing very good sensitivity and stability. The data is however very much impaired by man made emission in the protected band, leading to degraded measurements in several areas including parts of Europe and of China. However, many different international teams are now addressing cal val activities in various parts of the world, with notably large field campaigns either on the long time scale or over specific targets to address the specific issues. These campaigns take place in various parts of the world, in different environments from the Antarctic plateau to the deserts, from rain forests to deep oceans. Actually SMOS is a new sensor making new measurements paving the way to new applications. However it also requires a very fine analysis of the data so as to validate both the approach and the retrieval quality, as well as for monitoring the evolution of the sensor. To achieve such goals it is very important to link efficiently ground measurement to satellite measurements through field campaigns and related airborne acquisitions as well as with other existing sensors. This paper thus gives an overview of the science goals of the SMOS mission, a description of the main mission elements, and a foretaste of the first results including performances at brightness temperature as well as at geophysical parameters. It will include how the grond campaigns were elaborated to address the main cal Val activities accounting for SMOS specificities, in what context they were organized as well as the most significant results.}},2479 language = { Anglais},2480 affiliation = { Centre d'{\'e}tudes spatiales de la biosph{\`e}re - CESBIO , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Institut Pierre-Simon-Laplace - IPSL , Array Systems , European Space Research and Technology Centre - ESTEC , {\'E}cologie fonctionnelle et physique de l'environnement - EPHYSE - UR1263 , European State Research Institute - ESRIN , IFREMER - IFREMER , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2481 booktitle = {{PIERS Proceedings}},2473 title = {{SMOS {F}irst {R}esults {S}uccesses and {I}ssues: {T}owards {G}lobal {S}oil {M}oisture and {S}ea {S}ea {S}alinity {M}aps}}, 2474 author = {{Y}ann {H}. {K}err and {Ph}ilippe {W}aldteufel and {F}. {C}abot and P. {R}ichaume and A. {M}ahmoodi and {S}teven {D}elwart and {J}ean-{P}ierre {W}igneron and {S}. {M}ecklenburg and {N}icolas {R}eul and {J}acqueline {B}outin}, 2475 abstract = {{SMOS, a L {B}and radiometer using aperture synthesis to achieve a good spatial resolution, was successfully launched on {N}ovember 2, 2009. {I}t was developed and made under the leadership of the {E}uropean {S}pace {A}gency (ESA) as an {E}arth {E}xplorer {O}pportunity mission. {I}t is a joint program with the {C}entre {N}ational d'{E}tudes {S}patiales (CNES) in {F}rance and the {C}entro para el {D}esarrollo {T}eccnologico {I}ndustrial (CDTI) in {S}pain. SMOS carries a single payload, an L band 2D interferometric, radiometer in the 1400-1427 MHz h protected band. {T}his wavelength penetrates well through the vegetation and the atmosphere is almost transparent enabling to infer both soil moisture and vegetation water content over land and sea surface salinity over the oceans. SMOS achieves an unprecedented spatial resolution of 50 km at L-band maximum (43 km on average) with multi angular-dual polarized (or fully polarized) brightness temperatures over the globe and with a revisit time smaller than 3 days. SMOS as been now acquiring data for over one year after the end of the commissioning phase. {T}he data quality exceeds what was expected, showing very good sensitivity and stability. {T}he data is however very much impaired by man made emission in the protected band, leading to degraded measurements in several areas including parts of {E}urope and of {C}hina. {H}owever, many different international teams are now addressing cal val activities in various parts of the world, with notably large field campaigns either on the long time scale or over specific targets to address the specific issues. {T}hese campaigns take place in various parts of the world, in different environments from the {A}ntarctic plateau to the deserts, from rain forests to deep oceans. {A}ctually SMOS is a new sensor making new measurements paving the way to new applications. {H}owever it also requires a very fine analysis of the data so as to validate both the approach and the retrieval quality, as well as for monitoring the evolution of the sensor. {T}o achieve such goals it is very important to link efficiently ground measurement to satellite measurements through field campaigns and related airborne acquisitions as well as with other existing sensors. {T}his paper thus gives an overview of the science goals of the SMOS mission, a description of the main mission elements, and a foretaste of the first results including performances at brightness temperature as well as at geophysical parameters. {I}t will include how the grond campaigns were elaborated to address the main cal {V}al activities accounting for SMOS specificities, in what context they were organized as well as the most significant results.}}, 2476 language = {{A}nglais}, 2477 affiliation = {{C}entre d'études spatiales de la biosphère - CESBIO , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {A}rray {S}ystems , {E}uropean {S}pace {R}esearch and {T}echnology {C}entre - ESTEC , Écologie fonctionnelle et physique de l'environnement - EPHYSE - UR1263 , {E}uropean {S}tate {R}esearch {I}nstitute - ESRIN , IFREMER - IFREMER , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2478 booktitle = {{PIERS {P}roceedings}}, 2482 2479 pages = {590-593}, 2483 address = { Suzhou, Chine},2480 address = {{S}uzhou, {C}hine}, 2484 2481 audience = {internationale}, 2485 2482 year = {2011}, … … 2492 2489 loceanbibid = {01768}, 2493 2490 timestamp = {20121107}, 2494 title = {{BEAR, une station de mesure pour l'oc {\'e}an Arctique}},2495 author = { R. Loisil and {L}aurence {E}ymard and N. Amarouche and J.M. Panel and {A}ntonio {L}ourenço and A. Matulka and {A}lain {W}eill and {F}rédéric {V}ivier and Monique Dechambre and A. Viola and V. Vitale and S. Argentini and H. Kupfer},2496 abstract = {{Dans le cadre du projet ANR OPTIMISM, une station m {\'e}t{\'e}orologique a {\'e}t{\'e} mise au point afin d'acc{\'e}der au bilan d'{\'e}nergie dans l'oc{\'e}an Arctique via le couplage de cette station avec le syst{\`e}me ICE-T de d{\'e}termination de l'{\'e}paisseur de la glace (Ice Thickness determination). Les premiers essais technologiques et scientifiques de cette station nomm{\'e}e BEAR (Bilan d'{\'e}nergie arctique et recherche) sont d{\'e}crits. Des r{\'e}sultats pr{\'e}liminaires, obtenus lors d'une campagne exp{\'e}rimentale en avril-mai 2010 {\`a} Ny{\AA}lesund (Spitzberg) au-dessus d'une surface de neige/glace, sont notamment pr{\'e}sent{\'e}s et mis en perspective. A meteorological mast was developed in the framework of the OPTIMISM ANR project in order to get the energy budget in the Arctic Ocean when coupled with the ICE-T (Ice Thickness determination) system. First technological and scientific trials of this meteorological mast named the BEAR system (Budget of Energy for Arctic Research) are described. Preliminary results from an experiment at Ny-{\AA}lesund (Spitsbergen) in April-May 2010 over an ice/snow surface are more particularly presented and put into perspective.}},2497 keywords = { Interaction oc{\'e}an-atmosph{\`e}re; Observation m{\'e}t{\'e}orologique; Oc{\'e}an arctique; R{\'e}chauffement climatique; Fonte des glaciers; Bilan {\'e}nerg{\'e}tique; Vent; Temp{\'e}rature; Rayonnement},2498 language = { Fran{\c c}ais},2499 affiliation = { Institut National des Sciences de l'Univers - INSU/SPU , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Groupe d'{\'e}tude de l'atmosph{\`e}re m{\'e}t{\'e}orologique - CNRM-GAME , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Institut Pierre-Simon-Laplace - IPSL , Istituto di Scienze dell'Atmosfera e del Clima -- CNR},2491 title = {{BEAR, une station de mesure pour l'océan {A}rctique}}, 2492 author = {{R}. {L}oisil and {L}aurence {E}ymard and N. {A}marouche and J.M. {P}anel and {A}ntonio {L}ourenço and A. {M}atulka and {A}lain {W}eill and {F}rédéric {V}ivier and {M}onique {D}echambre and A. {V}iola and V. {V}itale and S. {A}rgentini and H. {K}upfer}, 2493 abstract = {{Dans le cadre du projet ANR OPTIMISM, une station météorologique a été mise au point afin d'accéder au bilan d'énergie dans l'océan {A}rctique via le couplage de cette station avec le système ICE-T de détermination de l'épaisseur de la glace (Ice {T}hickness determination). {L}es premiers essais technologiques et scientifiques de cette station nommée BEAR (Bilan d'énergie arctique et recherche) sont décrits. {D}es résultats préliminaires, obtenus lors d'une campagne expérimentale en avril-mai 2010 à {N}yÅlesund (Spitzberg) au-dessus d'une surface de neige/glace, sont notamment présentés et mis en perspective. A meteorological mast was developed in the framework of the OPTIMISM ANR project in order to get the energy budget in the {A}rctic {O}cean when coupled with the ICE-T (Ice {T}hickness determination) system. {F}irst technological and scientific trials of this meteorological mast named the BEAR system (Budget of {E}nergy for {A}rctic {R}esearch) are described. {P}reliminary results from an experiment at {N}y-Ålesund (Spitsbergen) in {A}pril-{M}ay 2010 over an ice/snow surface are more particularly presented and put into perspective.}}, 2494 keywords = {{I}nteraction océan-atmosphère; {O}bservation météorologique; {O}céan arctique; {R}échauffement climatique; {F}onte des glaciers; {B}ilan énergétique; {V}ent; {T}empérature; {R}ayonnement}, 2495 language = {{F}rançais}, 2496 affiliation = {{I}nstitut {N}ational des {S}ciences de l'{U}nivers - INSU/SPU , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {G}roupe d'étude de l'atmosphère météorologique - CNRM-GAME , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {I}stituto di {S}cienze dell'{A}tmosfera e del {C}lima -- CNR}, 2500 2497 pages = {23-34}, 2501 journal = { La M{\'e}t{\'e}orologie},2498 journal = {{L}a {M}étéorologie}, 2502 2499 number = {74}, 2503 2500 audience = {internationale}, … … 2511 2508 timestamp = {20121107}, 2512 2509 hal_id = {hal-00711272}, 2513 title = {{OCARINA : a new platform dedicated to measurements of Air-Sea fluxes}},2514 author = { Denis Bourras and Christophe Caudoux and Lucio Baggio and E. Luisset and Pierre Gilbert and Jean-Pierre Pineau and Jean-Jacques Correia and N. Geyskens and A. Clémençon and H. Branger and {L}aurent {M}ortier and {G}illes {R}everdin and L. Marié and Alain Weill and M. Berthet and A. Mironov},2515 abstract = {{OCARINA (Ocean Coupled with Atmosphere : Recherche Instrumentale sur Navire Annexe) is a small moving platform deployed from a research vessel. Turbulent fluxes, radiation fluxes, and wave state can all be derived from the instruments embedded on OCARINA, which include a sonic anemometer, an inertial platform, a CT probe, and other sensors. OCARINA was recently deployed during the FROMVAR experiment in Mer d'Iroise. It was successfully operated in winds up to 12 m/s and waves up to 4 m. The platform and datasets will be presented. Turbulent fluxes estimated with OCARINA data will be compared to data collected on the host vessel.}},2516 language = { Anglais},2517 affiliation = { Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Institut National des Sciences de l'Univers - INSU/SPU , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire de physique des oc{\'e}ans - LPO},2518 booktitle = {{EGU General Assembly 2012}},2519 address = { Vienna, Autriche},2520 audience = {non sp {\'e}cifi{\'e}e},2510 title = {{OCARINA : a new platform dedicated to measurements of {A}ir-{S}ea fluxes}}, 2511 author = {{D}enis {B}ourras and {C}hristophe {C}audoux and {L}ucio {B}aggio and E. {L}uisset and {P}ierre {G}ilbert and {J}ean-{P}ierre {P}ineau and {J}ean-{J}acques {C}orreia and N. {G}eyskens and A. {C}lémençon and H. {B}ranger and {L}aurent {M}ortier and {G}illes {R}everdin and L. {M}arié and {A}lain {W}eill and M. {B}erthet and A. {M}ironov}, 2512 abstract = {{OCARINA (Ocean {C}oupled with {A}tmosphere : {R}echerche {I}nstrumentale sur {N}avire {A}nnexe) is a small moving platform deployed from a research vessel. {T}urbulent fluxes, radiation fluxes, and wave state can all be derived from the instruments embedded on OCARINA, which include a sonic anemometer, an inertial platform, a CT probe, and other sensors. OCARINA was recently deployed during the FROMVAR experiment in {M}er d'{I}roise. {I}t was successfully operated in winds up to 12 m/s and waves up to 4 m. {T}he platform and datasets will be presented. {T}urbulent fluxes estimated with OCARINA data will be compared to data collected on the host vessel.}}, 2513 language = {{A}nglais}, 2514 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {I}nstitut {N}ational des {S}ciences de l'{U}nivers - INSU/SPU , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire de physique des océans - LPO}, 2515 booktitle = {{EGU {G}eneral {A}ssembly 2012}}, 2516 address = {{V}ienna, {A}utriche}, 2517 audience = {non spécifiée}, 2521 2518 year = {2012}, 2522 2519 } … … 2528 2525 timestamp = {20121107}, 2529 2526 hal_id = {hal-00712716}, 2530 title = {{Investigation of the ocean-atmosphere-continent coupling in the Gulf of Guinea and West Africa at intraseasonal timescales in boreal spring and summer with a regional atmospheric model (WRF)}},2527 title = {{Investigation of the ocean-atmosphere-continent coupling in the {G}ulf of {G}uinea and {W}est {A}frica at intraseasonal timescales in boreal spring and summer with a regional atmospheric model (WRF)}}, 2531 2528 author = {{R}émi {M}eynadier and {G}aëlle {{d}e {C}oëtlogon} and {M}arion {L}educ-{L}eballeur and {S}ophie {B}astin and {A}nne-{C}harlotte {P}eter and {S}erge {J}anicot and {O}livier {B}ock and {C}yrille {F}lamant}, 2532 abstract = {{Using 2000-2009 satellite data (Reynolds for SST and QuikSCAT for surface winds), a strong ocean-atmosphere coupling was put in evidence in the equatorial region (northern front) of the Tropical Atlantic cold tongue, implying surface winds and sea surface temperature (SST): a cold (respectively warm) SST anomaly strengthens (weakens) southerlies between the Equator and the Guinean coast during a few days. Similar investigations with ERA-Interim and NCEP-CFSR reanalyses emphasized the significant contribution of these wind fluctuations to the triggering of the Guinean coastal rainfall in spring. In this study, mechanisms at stake behind the statistical results are investigated by using a regional atmospheric model, WRF (Weather Research and Forecasting) with horizontal resolution of 50 km for the period April-July 2006. First, the influence of the SST on the spring and summer precipitation is quantified through the analysis of the moisture flux convergence over the continent. Then, some hints of a potential feedback from the changing continental surface (under rainy conditions) over the regional atmospheric circulation are shown , likely involving the southward low-level atmospheric circulation (or Shallow Meridional Circulation), subsidence over the Gulf of Guinea and then surface southerlies again, closing an active loop of ocean-atmosphere-continent interaction.}},2533 language = { Anglais},2534 affiliation = { Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire de Recherche en G{\'e}od{\'e}sie, IGN - LAREG , Universit{\'e} Paris 6, Pierre et Marie Curie - UPMC},2535 booktitle = {{EGU General Assembly 2012}},2536 address = { Vienna, Autriche},2537 audience = {non sp {\'e}cifi{\'e}e},2529 abstract = {{Using 2000-2009 satellite data (Reynolds for SST and {Q}uikSCAT for surface winds), a strong ocean-atmosphere coupling was put in evidence in the equatorial region (northern front) of the {T}ropical {A}tlantic cold tongue, implying surface winds and sea surface temperature (SST): a cold (respectively warm) SST anomaly strengthens (weakens) southerlies between the {E}quator and the {G}uinean coast during a few days. {S}imilar investigations with ERA-{I}nterim and NCEP-CFSR reanalyses emphasized the significant contribution of these wind fluctuations to the triggering of the {G}uinean coastal rainfall in spring. {I}n this study, mechanisms at stake behind the statistical results are investigated by using a regional atmospheric model, WRF (Weather {R}esearch and {F}orecasting) with horizontal resolution of 50 km for the period {A}pril-{J}uly 2006. {F}irst, the influence of the SST on the spring and summer precipitation is quantified through the analysis of the moisture flux convergence over the continent. {T}hen, some hints of a potential feedback from the changing continental surface (under rainy conditions) over the regional atmospheric circulation are shown , likely involving the southward low-level atmospheric circulation (or {S}hallow {M}eridional {C}irculation), subsidence over the {G}ulf of {G}uinea and then surface southerlies again, closing an active loop of ocean-atmosphere-continent interaction.}}, 2530 language = {{A}nglais}, 2531 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire de {R}echerche en {G}éodésie, IGN - LAREG , {U}niversité {P}aris 6, {P}ierre et {M}arie {C}urie - UPMC}, 2532 booktitle = {{EGU {G}eneral {A}ssembly 2012}}, 2533 address = {{V}ienna, {A}utriche}, 2534 audience = {non spécifiée}, 2538 2535 year = {2012}, 2539 2536 } … … 2545 2542 timestamp = {20121107}, 2546 2543 hal_id = {hal-00723829}, 2547 title = { The role of synoptic dry-air intrusions on the West African monsoon onset using observations and nudged climate simulations. Application to the monsoon onset of 2006},2544 title = {{T}he role of synoptic dry-air intrusions on the {W}est {A}frican monsoon onset using observations and nudged climate simulations. {A}pplication to the monsoon onset of 2006}, 2548 2545 author = {{E}mmanouil {F}laounas and {S}erge {J}anicot and {S}ophie {B}astin and {R}émy {R}oca and {E}lsa {M}ohino}, 2549 language = { Anglais},2550 affiliation = { Institut Pierre-Simon-Laplace - IPSL , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD},2551 booktitle = {{4th AMMA International Conference}},2552 address = { Toulouse, France},2553 audience = {non sp {\'e}cifi{\'e}e},2546 language = {{A}nglais}, 2547 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {L}aboratoire de {M}étéorologie {D}ynamique - LMD}, 2548 booktitle = {{4th AMMA {I}nternational {C}onference}}, 2549 address = {{T}oulouse, {F}rance}, 2550 audience = {non spécifiée}, 2554 2551 year = {2012}, 2555 2552 month = jun, … … 2561 2558 loceanbibid = {01764}, 2562 2559 timestamp = {20121107}, 2563 Author = { Simon Ruiz and Bartolome Garau and Miguel Martinez-Ledesma and Benjamin Casas and Ananda Pascual and Guillermo Vizoso and Jerome Bouffard and Emma Heslop and Alberto Alvarez and {P}ierre {T}estor and Joaquin Tintore},2564 Title = { New technologies for marine research: five years of glider activities at IMEDEA},2560 Author = {{S}imon {R}uiz and {B}artolome {G}arau and {M}iguel {M}artinez-{L}edesma and {B}enjamin {C}asas and {A}nanda {P}ascual and {G}uillermo {V}izoso and {J}erome {B}ouffard and {E}mma {H}eslop and {A}lberto {A}lvarez and {P}ierre {T}estor and {J}oaquin {T}intore}, 2561 Title = {{N}ew technologies for marine research: five years of glider activities at IMEDEA}, 2565 2562 Journal = {SCIENTIA MARINA}, 2566 2563 Year = {2012}, … … 2573 2570 2574 2571 @article{MasonColasEtAl:SM:2012, 2575 Author = { Evan Mason and {F}rançois {C}olas and Josep L. Pelegri},2576 Title = { A Lagrangian study tracing water parcel origins in the Canary Upwelling2572 Author = {{E}van {M}ason and {F}rançois {C}olas and {J}osep L. {P}elegri}, 2573 Title = {{A} {L}agrangian study tracing water parcel origins in the {C}anary {U}pwelling 2577 2574 System}, 2578 2575 Journal = {SCIENTIA MARINA}, … … 2594 2591 loceanbibid = {01762}, 2595 2592 timestamp = {20121107}, 2596 Author = { Meaghan K. Gorman and Terrence M. Quinn and Frederick W. Taylor and Judson W. Partin and {G}uy {C}abioch and James A. Jr Austin and Bernard Pelletier and Valerie Ballu and Christophe Maes and Steffen Saustrup},2597 Title = { A coral-based reconstruction of sea surface salinity at Sabine Bank, Vanuatu from 1842 to 2007 CE},2593 Author = {{M}eaghan K. {G}orman and {T}errence M. {Q}uinn and {F}rederick W. {T}aylor and {J}udson W. {P}artin and {G}uy {C}abioch and {J}ames A. {J}r {A}ustin and {B}ernard {P}elletier and {V}alerie {B}allu and {C}hristophe {M}aes and {S}teffen {S}austrup}, 2594 Title = {{A} coral-based reconstruction of sea surface salinity at {S}abine {B}ank, {V}anuatu from 1842 to 2007 CE}, 2598 2595 Journal = {PALEOCEANOGRAPHY}, 2599 2596 Year = {2012}, … … 2604 2601 } 2605 2602 2606 @article{Oliveira -SilvaBarbosaEtAl:MM:2012,2603 @article{OliveirasilvaBarbosaEtAl:MM:2012, 2607 2604 loceanteam={paleoproxus}, 2608 2605 loceanaffectation={ird}, 2609 2606 loceanbibid = {01761}, 2610 2607 timestamp = {20121107}, 2611 Author = { Patricia Oliveira-Silva and Catia Fernandes Barbosa and Carine Machado de Almeida and Jose Carlos Sicoli Seoane and Renato Campello Cordeiro and {B}runo {T}urcq and Abilio Soares-Gomes},2612 Title = { Sedimentary geochemistry and foraminiferal assemblages in coral reef assessment of Abrolhos, Southwest Atlantic},2608 Author = {{P}atricia {O}liveira-{S}ilva and {C}atia {F}ernandes {B}arbosa and {C}arine {M}achado de {A}lmeida and {J}ose {C}arlos {S}icoli {S}eoane and {R}enato {C}ampello {C}ordeiro and {B}runo {T}urcq and {A}bilio {S}oares-{G}omes}, 2609 Title = {{S}edimentary geochemistry and foraminiferal assemblages in coral reef assessment of {A}brolhos, {S}outhwest {A}tlantic}, 2613 2610 Journal = {MARINE MICROPALEONTOLOGY}, 2614 2611 Year = {2012}, … … 2624 2621 loceanbibid = {01760}, 2625 2622 timestamp = {20121107}, 2626 Author = { B. Dewitte and J. Vazquez-Cuervo and K. Goubanova and S. Illig and K. Takahashi and G. Cambon and S. Purca and D. Correa and D. Gutierrez and {A}bdelfettah {S}ifeddine and {L}uc {O}rtlieb},2627 Title = { Change in El Nino flavours over 1958-2008: Implications for the long-term trend of the upwelling off Peru},2623 Author = {{B}. {D}ewitte and J. {V}azquez-{C}uervo and K. {G}oubanova and S. {I}llig and K. {T}akahashi and G. {C}ambon and S. {P}urca and D. {C}orrea and D. {G}utierrez and {A}bdelfettah {S}ifeddine and {L}uc {O}rtlieb}, 2624 Title = {{C}hange in {E}l {N}ino flavours over 1958-2008: {I}mplications for the long-term trend of the upwelling off {P}eru}, 2628 2625 Journal = {DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY}, 2629 2626 Year = {2012}, … … 2634 2631 DOI = {10.1016/j.dsr2.2012.04.011}, 2635 2632 ISSN = {0967-0645}, 2636 Journal-ISO = { Deep-Sea Res. Part II-Top. Stud. Oceanogr.},2633 Journal-ISO = {{D}eep-{S}ea {R}es. {P}art II-{T}op. {S}tud. {O}ceanogr.}, 2637 2634 } 2638 2635 2639 2636 @article{SalvatteciFieldEtAl:P:2012, 2640 Author = {{R}enato {S}alvatteci and David B. Field and Timothy Baumgartner and Vicente Ferreira and Dimitri Gutierrez, Dimitri},2641 Title = { Evaluating fish scale preservation in sediment records from the oxygen minimum zone off Peru},2642 Journal = { Paleobiology},2637 Author = {{R}enato {S}alvatteci and {D}avid B. {F}ield and {T}imothy {B}aumgartner and {V}icente {F}erreira and {D}imitri {G}utierrez, {D}imitri}, 2638 Title = {{E}valuating fish scale preservation in sediment records from the oxygen minimum zone off {P}eru}, 2639 Journal = {{P}aleobiology}, 2643 2640 Year = {2012}, 2644 2641 Volume = {38}, … … 2659 2656 loceanbibid = {01758}, 2660 2657 timestamp = {20121106}, 2661 title = { Weighted Hierarchical Mixed Topological Map: une m{\'e}thode de classification hi{\'e}rarchique {\`a}deux niveaux},2662 author = { Mory Ouattara and Nd{\`e}ye Niang and {S}ylvie {T}hiria and Corinne Mandin and {F}ouad {B}adran},2663 language = { Fran{\c c}ais},2664 affiliation = { Centre d'Etude et De Recherche en Informatique du Cnam - CEDRIC , Centre Scientifique et Technique du B{\^a}timent - CSTB , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},2658 title = {{W}eighted {H}ierarchical {M}ixed {T}opological {M}ap: une méthode de classification hiérarchique à deux niveaux}, 2659 author = {{M}ory {O}uattara and {N}dèye {N}iang and {S}ylvie {T}hiria and {C}orinne {M}andin and {F}ouad {B}adran}, 2660 language = {{F}rançais}, 2661 affiliation = {{C}entre d'{E}tude et {D}e {R}echerche en {I}nformatique du {C}nam - CEDRIC , {C}entre {S}cientifique et {T}echnique du Bâtiment - CSTB , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 2665 2662 booktitle = {{EGC '2012}}, 2666 2663 pages = {10}, 2667 address = { bordeaux, France},2668 journal = { Fouille de Donn{\'e}es Complexes, complexit{\'e} li{\'e}e aux donn{\'e}es multiples et massives (FDC)},2664 address = {{B}ordeaux, {F}rance}, 2665 journal = {{F}ouille de {D}onnées {C}omplexes, complexité liée aux données multiples et massives (FDC)}, 2669 2666 volume = {12}, 2670 2667 audience = {nationale}, … … 2682 2679 loceanteam = {phybiocar}, 2683 2680 abstract = {{RATIONALE}: {I}n ecological studies of wildlife movements and foraging, bio-logging and isotopic data are routinely collected and increasingly analyzed in tandem. {S}uch analyses have two shortcomings: (1) small sample size linked with the number of telemetric tags that can be deployed, and (2) the observational nature of isotopic gradients. {W}ildlife ecologists are thus put in a statistical conundrum known as the small n, large p problem. METHODS: {U}sing shrinkage regression, which directly addresses the issue of accurately estimating effects from sparse data, we studied what counts as a biologically meaningful isotopic difference (a prerequisite to delineate isoscapes) in the southern elephant seal (Mirounga leonina), a large and elusive marine predator. RESULTS: {S}eals foraging in {A}ntarctic waters had a lower carbon isotopic value (by 2\%) than seals foraging either in the interfrontal zone or on the {K}erguelen {P}lateau. {T}he latter two foraging strategies were indistinguishable on the sole basis of d13C values with our data. CONCLUSIONS: {S}hrinkage regression is a conservative statistical technique that has wide applicability in isotopic ecology to help separate robust biological signals from noise}, 2684 language = { Anglais},2681 language = {{A}nglais}, 2685 2682 affiliation = {{C}entre d'études biologiques de {C}hizé - CEBC , {C}entre d'écologie fonctionnelle et évolutive - CEFE , LOCEAN-UPMC}, 2686 2683 pages = {2657-2664}, … … 2840 2837 booktitle={{C}ongrès {E}uropean {G}eophysical {U}nion}, 2841 2838 year={2011}, 2842 address = { Vienna, Autriche},2839 address = {{V}ienna, {A}utriche}, 2843 2840 aerestype={C-COM}, 2844 2841 aeresteam={mmsa}, … … 2853 2850 author={{D}oauda {D}iouf and {S}ylvie {T}hiria and {A}wa {N}iang and {J}ulien {B}rajard and {M}ichel {C}répon}, 2854 2851 title={{R}etrieving aerosol characteristics from satellite ocean color multi-spectral sensors using a neural-variational method}, 2855 booktitle={NCTA 2011 : NCTA- International Conference on Neural Computation Theory and Applications},2852 booktitle={NCTA 2011 : NCTA- {I}nternational {C}onference on {N}eural {C}omputation {T}heory and {A}pplications}, 2856 2853 year={2011}, 2857 2854 aerestype={C-COM}, … … 2867 2864 author = {{A}nastase {A}lexandre {C}harantonis and {J}ulien {B}rajard and {C}. {M}oulin and {F}ouad {B}adran and {S}ylvie {T}hiria}, 2868 2865 title={{I}nverse method for the retrieval of ocean vertical profiles using self-organizing maps and hidden {M}arkov models - {A}pplication on {O}cean {C}olour {S}atellite {I}mage {I}nversion}, 2869 booktitle={NCTA 2011 : NCTA- International Conference on Neural Computation Theory and Applications},2866 booktitle={NCTA 2011 : NCTA- {I}nternational {C}onference on {N}eural {C}omputation {T}heory and {A}pplications}, 2870 2867 year={2011}, 2871 2868 aerestype={C-COM}, … … 2882 2879 title={{I}nversion of sea surface data to retrieve the vertical distribution of phytoplankton using a statistical methodology}, 2883 2880 booktitle={{C}ongrès {E}uropean {G}eophysical {U}nion}, 2884 address = { Vienna, Autriche},2881 address = {{V}ienna, {A}utriche}, 2885 2882 year={2011}, 2886 2883 aerestype={C-COM}, … … 2896 2893 author = {{A}nastase {A}lexandre {C}harantonis and {S}ylvie {T}hiria and {C}. {M}oulin}, 2897 2894 title={{I}nfering the {C}hlorophyll-A {V}ertical {D}istribution in the {O}cean {F}rom {S}atellite {D}ata by {U}sing {H}idden {M}arkov {M}odels and {S}elf {O}rganizing {M}aps}, 2898 booktitle={ American Meteorological Society Annual Meeting},2895 booktitle={{A}merican {M}eteorological {S}ociety {A}nnual {M}eeting}, 2899 2896 address={{L}a {N}ouvelle {O}rléans}, 2900 2897 year={2012}, … … 2910 2907 author = {{M}ohamed {B}errada and {F}ouad {B}adran and {M}ichel {C}répon and {S}ylvie {T}hiria}, 2911 2908 title={A SOM-PCA {M}odel for {I}nverting {S}halow-{W}ater {A}coustic {D}ata}, 2912 booktitle={ American Meteorological Society Annual Meeting},2909 booktitle={{A}merican {M}eteorological {S}ociety {A}nnual {M}eeting}, 2913 2910 address={{L}a {N}ouvelle {O}rléans}, 2914 2911 year={2012}, … … 2933 2930 timestamp = {20121015}, 2934 2931 hal_id={hal-00750253}, 2935 address = { Vienna, Autriche},2932 address = {{V}ienna, {A}utriche}, 2936 2933 } 2937 2934 … … 3032 3029 abstract = {{N}ortheast {B}razil represents a key area in terms of {H}olocene environmental changes in {S}outh {A}merica due to its distinct semi-arid climate at near equatorial latitudes as well as to a wetter {E}arly and {M}iddle {H}olocene paleoclimate in comparison with other {S}outh {A}merica regions, which also experienced a reduced monsoon at that time. {W}e studied the lacustrine sediments of {L}ake {B}oqueirão, which is located at 5°S latitude on the {B}razilian {A}tlantic coast; it is directly influenced by displacement of the {I}ntertropical {C}onvergence {Z}one (ITCZ). A short (1 m) core "Boqc0701" was collected at a 7.5 m water depth during a seismic survey. {O}rganic matter (OM) geochemical [Rock {E}val {T}otal {O}rganic {C}arbon (TOC), {H}ydrogen {I}ndex (HI), {O}xygen {I}ndex (OI)] and petrographical studies allowed us to distinguish five sedimentary intervals during the last 3 kyrs. {P}hase E (3000 to 2050 cal yr BP) presents the largest TOC, HI and OI fluctuations in the entire core. {T}he most probable cause of these variations is a great instability in the lake level during this period. {P}hase D (2050 to 1830 cal yr BP) is marked by an increase in sedimentation rate and a higher contribution from a well-preserved OM with an algal origin; this was interpreted as a higher and more stable lake level. {D}uring phase C (1830 to 1550 cal yrs BP), low HI and high OI indicate the input of more oxidized, degraded and detrital OM, reflecting a lower lake level. {I}n phase B (1550 to 1470 cal yr BP), the OM quality and quantity (HI and TOC) indicate an algal contribution. {D}uring phase A (1470 to 570 cal yr BP), the high stability of the proxies may be due to a deep environment where OM fluctuations are strongly buffered. {T}hese changes in lake level can be compared with other tropical {S}outh {A}merica high resolution records. A correspondence seems to exist between phases of low ENSO, cool {N}orth {A}tlantic {O}cean and {B}oqueirão wet phases. {W}e did not encounter this same pattern during the last 1050 yaers, during which the 1050-570 cal yrs BP interval was generally wet (although probable fluctuations are buffered in our proxies) while the {N}orth {A}tlantic was warm (Mann et al., 2009). A prolonged dryness occurred in {L}ake {B}oqueirão from 570 cal yrs BP until recent decades. {T}his phase corresponds to the {L}ittle {I}ce {A}ge characterized by a cooler {N}orth {A}tlantic {O}cean (Mann et al., 2009). {T}hese data indicate that the teleconnection pattern between the tropical {A}tlantic, ENSO and {N}ortheast {B}razil rainfalls has changed in the past.}, 3033 3030 keywords = {{R}ock-{E}val, organic petrography, macrophytes, algal, intertropical convergence.}, 3034 language = { Anglais},3031 language = {{A}nglais}, 3035 3032 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , LMI "PALEOTRACES" , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {D}epartamento de {G}eoquìmica , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA}, 3036 3033 pages = {24 p.}, … … 3047 3044 title = {{I}mpact of the air-sea coupling in the {G}ulf of {G}uinea on the {G}uinean coastal water cycle in boreal spring}, 3048 3045 author = {{R}émi {M}eynadier and {G}aëlle {{d}e {C}oëtlogon} and {L}aurence {E}ymard and {M}arion {L}educ-{L}eballeur and {S}ophie {B}astin and {S}erge {J}anicot and {O}livier {B}ock and {C}yrille {F}lamant}, 3049 language = { Anglais},3046 language = {{A}nglais}, 3050 3047 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {U}niversité {P}aris 6, {P}ierre et {M}arie {C}urie - UPMC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratoire de {R}echerche en {G}éodésie, IGN - LAREG}, 3051 3048 booktitle = {4th {AMMA} {I}nternational {C}onference}, … … 3064 3061 hal_id={hal-00723388}, 3065 3062 title = {{A}ir-sea interaction in the {G}ulf of {G}uinea at intraseasonal timescales : A quasi-biweekly oscillation in the eastern equatorial {A}tlantic}, 3066 language = { Anglais},3063 language = {{A}nglais}, 3067 3064 affiliation = {{I}nstitut {P}ierre-{S}imon-{L}aplace - IPSL , {L}aboratoire {A}tmosphères, {M}ilieux, {O}bservations {S}patiales - LATMOS , {U}niversité {P}aris 6, {P}ierre et {M}arie {C}urie - UPMC , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 3068 3065 booktitle = {4th {AMMA} {I}nternational {C}onference}, … … 3081 3078 journal = {{Z}ooKeys}, 3082 3079 publisher = {{P}ensoft {P}ublishers}, 3083 title = { Arevision of the genus {K}aszabister {M}azur (Histeridae, Histerinae, {E}xosternini)},3080 title = {{A} revision of the genus {K}aszabister {M}azur (Histeridae, Histerinae, {E}xosternini)}, 3084 3081 year = {2012}, 3085 3082 month = jun, … … 3446 3443 @conference{Lourantou:SOCAT:2010, 3447 3444 author = {{A}nna {L}ourantou}, 3448 title={ Islands of the subantarctic region},3445 title={{I}slands of the subantarctic region}, 3449 3446 booktitle={{S}outhern {O}cean SOCAT meeting}, 3450 3447 year = {2010}, … … 5306 5303 5307 5304 @UNPUBLISHED{NishaLengaigneEtAl:OD:2012submitted, 5308 author = {{K}. {N}isha and {M}atthieu {L}engaigne and {V}. {V}. {G}opalakrishna and {J}érôme {V}ialard and {S}téphane {P}ous and {A}nne-{C}harlotte {P}eter and {F}. {D}urand {S}. {N}aik},5305 author = {{K}. {N}isha and {M}atthieu {L}engaigne and {V}. {V}. {G}opalakrishna and {J}érôme {V}ialard and {S}téphane {P}ous and {A}nne-{C}harlotte {P}eter and {F}. {D}urand and {S}. {N}aik}, 5309 5306 title = {{P}rocesse of summer intraseasonal sea surface temperature variability along the coasts of {I}ndia}, 5310 5307 note = {submitted}, … … 6028 6025 6029 6026 @ARTICLE{BarrosGalassoEtAl:VJ:2011, 6030 author = {{M}aria CES {B}arros and {T}atiane {GCM} {G}alasso and {A}ntônio JM {C}haib and {N}icolas {D} egallier and {T}atsuya {N}agata and {B}ergmann {M}. {R}ibeiro},6027 author = {{M}aria CES {B}arros and {T}atiane {GCM} {G}alasso and {A}ntônio JM {C}haib and {N}icolas {D}égallier and {T}atsuya {N}agata and {B}ergmann {M}. {R}ibeiro}, 6031 6028 title = {{Y}ellow fever virus envelope protein expressed in insect cells is capable of syncytium formation in lepidopteran cells and could be used for immuno detection of {YFV} in human sera}, 6032 6029 journal = {{V}irology {J}ournal}, … … 7094 7091 year = {2011}, 7095 7092 pages = {291-292}, 7096 affiliation = {{C}entre d'études biologiques de {C}hizé - CEBC , Département {M}ilieux7093 affiliation = {{C}entre d'études biologiques de {C}hizé - CEBC , {D}épartement {M}ilieux 7097 7094 et {P}euplements {A}quatiques, MNHN}, 7098 7095 hal_id = {hal-00624588}, 7099 language = { English},7096 language = {{E}nglish}, 7100 7097 loceanbibid = {01551}, 7101 7098 loceanteam= {phybiocar}, … … 9748 9745 aerestype = {ACL}, 9749 9746 doi = {10.1007/s00382-011-1247-2}, 9750 Volume={39},9747 volume={39}, 9751 9748 number={3-4}, 9752 9749 pages={681-707}, … … 11187 11184 title = {{T}he role of the intra-daily {SST} variability in the {I}ndian monsoon variability and monsoon-{ENSO}-{IOD} relationships in a global coupled model}, 11188 11185 year = {2012}, 11189 Volume={39},11186 volume={39}, 11190 11187 number={3-4}, 11191 11188 Pages={729-754}, … … 25398 25395 aerestype = {PV}, 25399 25396 aeresteam = {varclim}, 25400 loceanaffectation = {ird,Météo- France},25397 loceanaffectation = {ird,Météo-{F}rance}, 25401 25398 loceanbibid = {00612}, 25402 25399 loceanteam = {varclim}, … … 26108 26105 doi = {10.1007/s00382-006-0215-8}, 26109 26106 language = {{A}nglais}, 26110 loceanaffectation = {ird,Météo- France},26107 loceanaffectation = {ird,Météo-{F}rance}, 26111 26108 loceanbibid = {00582}, 26112 26109 loceanteam={varclim}, … … 27282 27279 doi = {10.1007/s00382-006-0192-y}, 27283 27280 language = {{A}nglais}, 27284 loceanaffectation = {ird,Météo- France},27281 loceanaffectation = {ird,Météo-{F}rance}, 27285 27282 loceanbibid = {00528}, 27286 27283 loceanteam = {varclim}, … … 30335 30332 @PHDTHESIS{Contador:these:2005, 30336 30333 author = {{L}uciana {C}ontador}, 30337 title = {Étude de la structure chimique et microbiologique de linterface air-mer en Baie de Guanabara (Brésil)},30334 title = {Étude de la structure chimique et microbiologique de linterface air-mer en {B}aie de {G}uanabara (Brésil)}, 30338 30335 year = {2005}, 30339 30336 type = {{T}hèse de doctorat}, … … 32177 32174 @PHDTHESIS{Treignier:these:2005, 32178 32175 author = {{C}laire {T}reignier}, 32179 title = { Apports en matière organique marine et terrigène sur la marge équatoriale ouest africaine : rôle joué par le canyon sous-marin du Zaïre. Approche par les biomarqueurs lipidiques},32176 title = {{A}pports en matière organique marine et terrigène sur la marge équatoriale ouest africaine : rôle joué par le canyon sous-marin du {Z}aïre. {A}pproche par les biomarqueurs lipidiques}, 32180 32177 school = {{U}niversité de {P}aris {VI}}, 32181 32178 year = {2005}, … … 32509 32506 @ARTICLE{BoutinWaldteufelEtAl:JAOT:2004, 32510 32507 author = {{J}acqueline {B}outin and {Ph}ilippe {W}aldteufel and {N}icolas {M}artin and {G}érard {C}audal and {E}mmanuel {D}innat}, 32511 title = { Surface Salinity Retrieved from SMOS Measurements over the Global Ocean: Imprecisions Due to Sea Surface Roughness and Temperature Uncertainties},32508 title = {{S}urface {S}alinity {R}etrieved from SMOS {M}easurements over the {G}lobal {O}cean: {I}mprecisions {D}ue to {S}ea {S}urface {R}oughness and {T}emperature {U}ncertainties}, 32512 32509 journal = {{J}ournal of {A}tmospheric and {O}ceanic {T}echnology}, 32513 32510 year = {2004}, … … 33774 33771 timestamp = {20120419}, 33775 33772 hal_id = {hal-00153947}, 33776 comment = {20121115 : mauvais ordre auteurs dans hal hal-00153947 Laurent Mortier <mortier@locean-ipsl.upmc.fr>},33773 comment = {20121115 : mauvais ordre auteurs dans hal hal-00153947 {L}aurent {M}ortier <mortier@locean-ipsl.upmc.fr>}, 33777 33774 } 33778 33775 … … 34189 34186 hal_id={hal-00155070}, 34190 34187 comment = {20121114 : ++ compléter prénom dans hal}, 34191 comment = {20121114 : mauvaise liste auteur dans doublon hal-00270746 de Francoise Cudennec <Francoise.Cudennec@ird.fr>},34188 comment = {20121114 : mauvaise liste auteur dans doublon hal-00270746 de {F}rancoise {C}udennec <Francoise.Cudennec@ird.fr>}, 34192 34189 } 34193 34190
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