Changeset 299 for branches

Timestamp:

01/02/13 11:47:25 (11 years ago)

Author:

pinsard

Message:

add some ref thanks to wok

File:

• branches/bibliolocean/data/biblioref.bib (modified) (5 diffs)

branches/bibliolocean/data/biblioref.bib

@@ -3 +3 @@
 
 @PREAMBLE{"Bibliographie du LOCEAN"}
+
+@article{SaracenoProvost:DSR:2012,
+hal_id = {hal-00769553},
+loceanaffectation = {cnrs},
+loceanbibid = {01930},
+loceanteam = {paleoproxus},
+timestamp = {20130102},
+title = {{On eddy polarity distribution in the southwestern Atlantic}},
+author = {Martin Saraceno and {C}hristine {P}rovost},
+abstract = {{Not Available}},
+language = {Anglais},
+affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},
+pages = {62-69},
+journal = {Deep Sea Research Part I: Oceanographic Research Papers},
+volume = {69},
+audience = {internationale},
+doi = {10.1016/J.DSR.2012.07.005},
+year = {2012},
+month = nov,
+ads={2012DSRI...69...62S},
+}
+
+@article{LangehaugRhinesEtAl:JGR:2012,
+hal_id = {hal-00769550},
+loceanaffectation = {ird},
+loceanbibid = {01929},
+loceanteam = {paleoproxus},
+timestamp = {20130102},
+title = {{Water mass transformation and the North Atlantic Current in three multicentury climate model simulations}},
+author = {H. R. Langehaug and P. B. Rhines and T. Eldevik and Juliette Mignot and K. Lohmann},
+abstract = {{The warm and saline Subtropical Water carried by the North Atlantic Current undergoes substantial transformation on its way to higher latitudes, predominantly from oceanic heat loss to the atmosphere. The geographical distribution of the surface forced water mass transformation is assessed in multicentury climate simulations from three different climate models (BCM, IPSLCM4, and MPI-M ESM), with a particular focus on the eastern subpolar North Atlantic Ocean. A diagnosis, originally introduced by Walin (1982), estimates the surface water mass transformation from buoyancy forcing. While the depth structure of the Atlantic Meridional Overturning Circulation (AMOC) is similar in all models, their climatological heat and freshwater fluxes are very different. Consistently, the models differ in their mean pathways of the North Atlantic Current, location of upper ocean low salinity waters, as well as in sea ice cover. In the two models with an excessive sea ice extent in the Labrador Sea, most of the water mass transformation in the subpolar region occurs in the eastern part (east of 35\degreW). The variability of the eastern water mass transformation on decadal time scales is related to the variable warm northward flow into the subpolar region, the upper branch of AMOC, where a strengthened flow leads an intensified transformation. This relationship seems to disappear with a weak connection between the Subtropical and Subpolar gyres.}},
+keywords = {Oceanography: Physical: Air/sea interactions (0312;3339);Oceanography: Physical: Decadal ocean variability (1616;1635;3305;4215);},
+language = {Anglais},
+affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},
+pages = {11001},
+journal = {Journal of Geophysical Research},
+volume = {117},
+audience = {internationale},
+doi = {10.1029/2012JC008021},
+year = {2012},
+month = nov,
+ads={2012JGRC..11711001L},
+}
+
+@article{RayGiese:JGR:2012,
+hal_id = {hal-00769548},
+loceanbibid = {01928},
+loceanteam = {varclim},
+timestamp = {20130102},
+title = {{Historical changes in El Ni{\\~n}o and La Ni{\\~n}a characteristics in an ocean reanalysis}},
+author = {{S}ulagna {R}ay and Benjamin S. Giese},
+abstract = {{The variation of El Ni{\\~n}o Southern Oscillation (ENSO) events from the mid-nineteenth century until the beginning of the twenty-first century is explored using an ocean reanalysis. A comparison of the reanalysis with three sea surface temperature reconstructions shows that the timing of events is similar in all four products, however there are important differences in the strength and location of events. The difference between the reconstructions is sometimes larger than the difference between the reanalysis and a given reconstruction. These differences are larger in the first half of the record, a period for which there are relatively sparse observations. The reanalysis is used to explore decadal variability and trends in the frequency, duration, and propagation direction of ENSO events. There is considerable decadal variability of these ENSO characteristics with the time between events ranging from several months to ten years and the duration of ENSO varying from 5 to 27 months. As has been previously shown for the strength and location of ENSO there is little overall trend in the characteristics. Having a three dimensional representation of the ocean from the reanalysis allows exploration of subsurface changes during ENSO. An analysis of subsurface anomalies shows that during ENSO events the subsurface anomalies are highly correlated with the strength of surface anomalies over the 140 year period. Overall, there is no evidence that there are changes in the strength, frequency, duration, location or direction of propagation of El Ni{\\~n}o and La Ni{\\~n}a anomalies caused by global warming during the period from 1871 to 2008.}},
+keywords = {Global Change: Climate variability (1635;3305;3309;4215;4513);Global Change: Global climate models (3337;4928);Oceanography: General: Ocean data assimilation and reanalysis (3225);Oceanography: Physical: Decadal ocean variability (1616;1635;3305;4215);Oceanography: Physical: ENSO (4922);},
+language = {Anglais},
+affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},
+pages = {11007},
+journal = {Journal of Geophysical Research},
+volume = {117},
+audience = {internationale},
+doi = {10.1029/2012JC008031},
+year = {2012},
+month = nov,
+ads={2012JGRC..11711007R},
+}
+
+@article{DupreyLazarethEtAl:P:2012,
+hal_id = {hal-00769544},
+loceanaffectation = {ird},
+loceanbibid = {01927},
+loceanteam = {paleoproxus},
+timestamp = {20130102},
+title = {{Early mid-Holocene SST variability and surface-ocean water balance in the southwest Pacific}},
+author = {N. Duprey and {C}laire {E}. {L}azareth and Thierry Corrège and {F}lorence {{L}e Cornec} and C. Maes and N. Pujol and {M}agloire {M}andeng-{Y}ogo and {S}andrine {C}aquineau and C. Soares Derome and {G}uy {C}abioch},
+
+
+abstract = {{We present early mid-Holocene records of Sr/Ca, $\delta$18O and $\delta$18Osw from marine archives collected in Vanuatu: two Porites sp. corals (6.7-6.5 ka BP) and a Tridacna maxima giant clam (6.2-6.0 ka BP). Sr/Ca, $\delta$18O, and $\delta$18Osw were used as proxies for sea surface temperature (SST) and sea surface salinity (SSS). The fossil geochemical records were compared to modern Porites sp. and T. maxima records. Reconstructed mean SSTs from the two fossil Porites sp. and from the modern coral are similar, implying that the Western Pacific Warm Pool (WPWP)' southern edge had reached its modern location by 6.7-6.5 ka BP. The post-glacial SST rise in the Southwest Pacific was thus completed by the early mid-Holocene. The two early mid-Holocene corals and the giant clam recorded saltier conditions than modern related to 1) a decoupling between the precipitation regime and the SPCZ due to a northerly position of this climatic feature and 2) an increase of the moisture transport to the extra-tropics, driven by a strengthened or extended Hadley cell. The longest $\delta$18O coral profile displays an El Ni{\\~n}o Southern Oscillation (ENSO) signal reduced by 20-30\% compared to the period 1928-1992, in concordance with the reduced ENSO variability observed in the Pacific area during the first half of the Holocene. However, the decoupling between the SPCZ and the precipitation regime may have also contributed to the weak ENSO signal recorded in the early mid-Holocene coral $\delta$18O profile.}},
+keywords = {Biogeosciences: Paleoclimatology and paleoceanography (3344;4900);Atmospheric Processes: Paleoclimatology (0473;4900);},
+language = {Anglais},
+affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire d'{\'e}tudes en G{\'e}ophysique et oc{\'e}anographie spatiales - LEGOS},
+pages = {4207},
+journal = {Paleoceanography},
+volume = {27},
+audience = {internationale},
+doi = {10.1029/2012PA002350},
+year = {2012},
+month = nov,
+ads={2012PalOc..27.4207D},
+}
+
+@article{AzzougCarreEtAl:GPC:2012,
+hal_id = {hal-00769536},
+loceanaffectation = {ird,upmc},
+loceanbibid = {01926},
+loceanteam = {paleoproxus,varclim},
+timestamp = {20130102},
+title = {{Positive precipitation-evaporation budget from AD 460 to 1090 in the Saloum Delta (Senegal) indicated by mollusk oxygen isotopes}},
+author = {Moufok Azzoug and Matthieu Carré and Brian M. Chase and Abdoulaye Deme and {A}lban {L}azar and {C}laire {E}. {L}azareth and Andrew J. Schauer and {M}agloire {M}andeng-{Y}ogo and Monique Simier and Amadou Thierno-Gaye and Luis Tito De Morais},
+language = {Anglais},
+affiliation = {Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Ecosyst{\`e}mes marins exploit{\'e}s - EME},
+pages = {54-62},
+journal = {Global and Planetary Change},
+volume = {98},
+audience = {internationale},
+doi = {10.1016/J.GLOPLACHA.2012.08.003},
+year = {2012},
+month = dec,
+ads={2012GPC....98...54A},
+}
+
+@article{CarrilMenendezEtAl:CD:2012,
+hal_id = {hal-00769535},
+loceanaffectation = {cnrs},
+loceanbibid = {01925},
+loceanteam = {paleoproxus},
+timestamp = {20130102},
+title = {{Performance of a multi-{RCM} ensemble for South Eastern South America}},
+author = {A. F. Carril and C. G. Menéndez and A. R. C. Remedio and F. Robledo and A. Sörensson and B. Tencer and {J}ean-{P}hilippe {B}oulanger and M. De Castro and D. Jacob and Hervé Le Treut and L. Z. X. Li and O. Penalba and S. Pfeifer and M. Rusticucci and P. Salio and P. Samuelsson and E. Sanchez and P. Zaninelli},
+abstract = {{The ability of four regional climate models to reproduce the present-day South American climate is examined with emphasis on La Plata Basin. Models were integrated for the period 1991-2000 with initial and lateral boundary conditions from ERA-40 Reanalysis. The ensemble sea level pressure, maximum and minimum temperatures and precipitation are evaluated in terms of seasonal means and extreme indices based on a percentile approach. Dispersion among the individual models and uncertainties when comparing the ensemble mean with different climatologies are also discussed. The ensemble mean is warmer than the observations in South Eastern South America (SESA), especially for minimum winter temperatures with errors increasing in magnitude towards the tails of the distributions. The ensemble mean reproduces the broad spatial pattern of precipitation, but overestimates the convective precipitation in the tropics and the orographic precipitation along the Andes and over the Brazilian Highlands, and underestimates the precipitation near the monsoon core region. The models overestimate the number of wet days and underestimate the daily intensity of rainfall for both seasons suggesting a premature triggering of convection. The skill of models to simulate the intensity of convective precipitation in summer in SESA and the variability associated with heavy precipitation events (the upper quartile daily precipitation) is far from satisfactory. Owing to the sparseness of the observing network, ensemble and observations uncertainties in seasonal means are comparable for some regions and seasons.}},
+keywords = {Regional climate models;Multi-RCM ensemble validation;South Eastern South America;South America;},
+language = {Anglais},
+affiliation = {Centro de Investigaciones del Mar y la Atm{\'o}sfera/CONICET-UBA , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Max-Planck Institute for Meteorology , Laboratoire de M{\'e}t{\'e}orologie Dynamique - LMD , Max-Planck-Institute for Meteorology , Dpto. Matema'tica Aplicada, E.T.S. Ingenieros Industriales},
+pages = {2747-2768},
+journal = {Climate Dynamics},
+volume = {39},
+audience = {internationale},
+doi = {10.1007/S00382-012-1573-Z},
+year = {2012},
+month = dec,
+ads={2012ClDy...39.2747C},
+}
+
+@article{PierreBlancvalleronEtAl:GML:2012,
+hal_id = {hal-00769534},
+loceanaffectation = {cnrs},
+loceanbibid = {01924},
+loceanteam = {paleoproxus},
+timestamp = {20130102},
+title = {{Authigenic carbonates from active methane seeps offshore southwest Africa}},
+author = {{C}atherine {P}ierre and Marie-Madeleine Blanc-Valleron and Jérôme Demange and Omar Boudouma and Jean-Paul Foucher and Thomas Pape and Tobias Himmler and Noemi Fekete and Volkhard Spiess},
+abstract = {{The southwest African continental margin is well known for occurrences of active methane-rich fluid seeps associated with seafloor pockmarks at water depths ranging broadly from the shelf to the deep basins, as well as with high gas flares in the water column, gas hydrate accumulations, diagenetic carbonate crusts and highly diverse benthic faunal communities. During the M76/3a expedition of R/V METEOR in 2008, gravity cores recovered abundant authigenic carbonate concretions from three known pockmark sites--Hydrate Hole, Worm Hole, the Regab pockmark--and two sites newly discovered during that cruise, the so-called Deep Hole and Baboon Cluster. The carbonate concretions were commonly associated with seep-benthic macrofauna and occurred within sediments bearing shallow gas hydrates. This study presents selected results from a comprehensive analysis of the mineralogy and isotope geochemistry of diagenetic carbonates sampled at these five pockmark sites. The oxygen isotope stratigraphy obtained from three cores of 2-5 m length indicates a maximum age of about 60,000-80,000 years for these sediments. The authigenic carbonates comprise mostly magnesian calcite and aragonite, associated occasionally with dolomite. Their very low carbon isotopic compositions (-61.0 < $\delta$13C # V-PDB < -40.1) suggest anaerobic oxidation of methane (AOM) as the main process controlling carbonate precipitation. The oxygen isotopic signatures (+2.4 < $\delta$18O # V-PDB < +6.2) lie within the range in equilibrium under present-day/interglacial to glacial conditions of bottom seawater; alternatively, the most positive $\delta$18O values might reflect the contribution of 18O-rich water from gas hydrate decomposition. The frequent occurrence of diagenetic gypsum crystals suggests that reduced sulphur (hydrogen sulphide, pyrite) from sub-seafloor sediments has been oxidized by oxygenated bottom water. The acidity released during this process can potentially induce the dissolution of carbonate, thereby providing enough Ca2+ ions for pore solutions to reach gypsum saturation; this is thought to be promoted by the bio-irrigation and burrowing activity of benthic fauna. The $\delta$18O-$\delta$13C patterns identified in the authigenic carbonates are interpreted to reflect variations in the rate of AOM during the last glacial-interglacial cycle, in turn controlled by variably strong methane fluxes through the pockmarks. These results complement the conclusions of Kasten et al. in this special issue, based on authigenic barite trends at the Hydrate Hole and Worm Hole pockmarks which were interpreted to reflect spatiotemporal variations in AOM related to subsurface gas hydrate formation-decomposition.}},
+language = {Anglais},
+affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Institut des Sciences de la Terre de Paris - iSTeP , D{\'e}partement G{\'e}osciences Marines},
+pages = {501-513},
+journal = {Geo-Marine Letters},
+volume = {32},
+audience = {internationale},
+doi = {10.1007/S00367-012-0295-X},
+year = {2012},
+month = dec,
+ads={2012GML....32..501P},
+}
 
 @article{VialardDrushkaEtAl:CD:2012,
@@ -386 +537 @@
 loceanbibid = {01903},
 timestamp={20121115},
-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)).}},
+title = {{A 36 ka environmental record in the southern tropics : {L}ake {T}ritrivakely ({M}adgascar) (Un enregistrement de l'environnement depuis 36 ka en zone tropicale sud : le lac {T}ritrivakely ({M}adagascar)).}},
 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},
 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}},
@@ -2464 +2615 @@
 title = {{Linking {O}cean {V}ariabilty to {P}hytoplankton {C}hanges {O}ver the {L}ast 2000 {Y}ears off N. {I}celand}},
 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},
-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.}},
 language = {{A}nglais},
 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},
@@ -2893 +3043 @@
 }
 
-@unpublished{BrajardSanterEtAl:RSE:2012inrevision,
+@article{BrajardSanterEtAl:RSE:2012,
 author = {{J}ulien {B}rajard and {R}. {S}anter and {M}ichel {C}répon and {S}ylvie {T}hiria},
 title={{A}tmospheric correction of MERIS data for case 2 waters using a neuro-variational inversion},
-journal={RSE},
-note={in revision},
+journal={Remote Sensing of environment},
 year={2012},
-format = {in revision},
+volume={126},
+pages={51-61},
+doi={10.1016/j.rse.2012.07.004},
 loceanteam={mmsa},
 loceanaffectation={uvsq,upmc,cnrs},
@@ -7779 +7930 @@
 
 @CONFERENCE{DupreyPujolEtAl:AGU:2011,
-  author = {{N}. {D}uprey and {N}. {P}ujol and {C}laire {E}. {L}azareth and {G}uy {C}abioch and {T}. {C}orrège and {F}lorence {{L}e {C}ornec} and {C}. {M}aes and {J}.-{C}. {G}alipaud and {S}andrine {C}aquineau and {M}agloire {M}adeng-{Y}ogo},
+  author = {{N}. {D}uprey and {N}. {P}ujol and {C}laire {E}. {L}azareth and {G}uy {C}abioch and {T}. {C}orrège and {F}lorence {{L}e {C}ornec} and {C}. {M}aes and {J}.-{C}. {G}alipaud and {S}andrine {C}aquineau and {M}agloire {M}andeng-{Y}ogo},
   title = {{S}outh {W}est {P}acific climate at c. 6600-6000 BP inferred from giant clam {T}ridacna maxima and massive coral {P}orites sp. records},
   booktitle = {{AGU} {F}all {M}eeting 2011},