Changeset 342


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Timestamp:
08/05/13 13:33:31 (11 years ago)
Author:
pinsard
Message:

a new ref thanks to HAL

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1 edited

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  • branches/bibliolocean/data/biblioref.bib

    r341 r342  
    33 
    44@PREAMBLE{"Bibliographie du LOCEAN"} 
     5 
     6@article{ReverdinMorissetEtAl:O:2013, 
     7  loceanbibid = {01976}, 
     8  loceanaffectation = {cnrs}, 
     9  loceanteam = {surf,ditm}, 
     10  timestamp = {20130805}, 
     11    hal_id = {hal-00850053}, 
     12    url = {http://hal.archives-ouvertes.fr/hal-00850053}, 
     13    title = {{Surpact: A SMOS Surface Wave Rider for Air-Sea Interaction}}, 
     14    author = {Reverdin, Gilles and Morisset, Simon and Bourras, Denis and Martin, Nicolas and Lourenço, Antonio and Boutin, Jacqueline and Caudoux, C. and Font, J. and Salvador, J.}, 
     15    abstract = {{A new small wave rider called Surpact was developed for air-sea investigations. It was designed to attach to a drifter or a mooring and to float upon the surface waves in order to measure sea state and atmospheric sea level pressure as well as temperature and salinity at a small fixed depth from the surface. Wind speed is derived from Surpact sea state measurements, and the data are calibrated with co-located Special Sensor Microwave Imager Sounder (SSMIS) wind retrievals during a four-month deployment in the North Atlantic subtropics. Individual 15-minute wind estimates present a root mean square difference on the order of 15\% with the SSMIS wind retrievals for wind speeds less than 12 m s-1. The wind retrievals might lag the actual wind changes for moderate to strong winds by an hour. This article discusses the accuracy of these wind retrievals based on in situ data collected during the Strasse cruise in August and September 2012. Temperature and salinity data are also examined. The authors find, under some sunny conditions, radiative warming of the temperature probe reduces the accuracy of some of the daytime temperature data and also affects corresponding salinity estimates. Nonetheless, small realistic daily cycles of near-surface salinity (0.01 psu amplitude) were observed. Also, examples of wind time series collected during salinity drops caused by rainfall during late 2012 in the North Atlantic subtropics indicate no intensification of wind during these rain events.}}, 
     16    keywords = {Pacific warm pool; Salinity measurements}, 
     17    language = {Anglais}, 
     18    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 , Institute of Marine Sciences / Institut de Ci{\`e}ncies del Mar [Barcelona] - ICM}, 
     19    pages = {48-57}, 
     20    journal = {Oceanography}, 
     21    volume = {26}, 
     22    number = {1}, 
     23    audience = {internationale}, 
     24    doi = {10.5670/oceanog.2013.04}, 
     25    year = {2013}, 
     26} 
     27 
     28@article{KurianLengaigneEtAl:OD:2013, 
     29  loceanbibid = {01975}, 
     30  loceanaffectation = {ird}, 
     31  loceanteam = {varclim}, 
     32  timestamp = {20130725}, 
     33    hal_id = {hal-00848066}, 
     34    title = {{Processes of India's offshore summer intraseasonal sea surface temperature variability}}, 
     35    author = {Kurian, Nisha and Lengaigne, Matthieu and Vissa, Gopalakrishna Venkata and Vialard, Jérôme and Pous, Stéphane and Peter, Anne-Charlotte and Durand, Fabien and Naik, Shweta}, 
     36    abstract = {{Active and break phases of the Indian summer monsoon are associated with sea surface temperature (SST) fluctuations at 30-90 days timescale in the Arabian Sea and Bay of Bengal. Mechanisms responsible for basin-scale intraseasonal SST variations have previously been discussed, but the maxima of SST variability are actually located in three specific offshore regions: the South-Eastern Arabian Sea (SEAS), the Southern Tip of India (STI) and the North-Western Bay of Bengal (NWBoB). In the present study, we use an eddy-permitting 0.25\degre regional ocean model to investigate mechanisms of this offshore intraseasonal SST variability. Modelled climatological mixed layer and upper thermocline depth are in very good agreement with estimates from three repeated expendable bathythermograph transects perpendicular to the Indian Coast. The model intraseasonal forcing and SST variability agree well with observed estimates, although modelled intraseasonal offshore SST amplitude is undere-stimated by 20-30 \%. Our analysis reveals that surface heat flux variations drive a large part of the intraseasonal SST variations along the Indian coastline while oceanic processes have contrasted contributions depending of the region considered. In the SEAS, this contribution is very small because intraseasonal wind variations are essentially cross-shore, and thus not associated with significant upwelling intraseasonal fluctuations. In the STI, vertical advection associated with Ekman pumping contributes to ~30 \% of the SST fluctuations. In the NWBoB, vertical mixing diminishes the SST variations driven by the atmospheric heat flux perturbations by 40 \%. Simple slab ocean model integrations show that the amplitude of these intraseasonal SST signals is not very sensitive to the heat flux dataset used, but more sensitive to mixed layer depth.}}, 
     37    keywords = {Indian Ocean;Intraseasonal variability;Sea surface temperature;Regional ocean model;Oceanic and atmospheric processes;}, 
     38    language = {Anglais}, 
     39    affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire d'Etudes en G{\'e}ophysique et Oc{\'e}anographie Spatiales - LEGOS}, 
     40    pages = {329-346}, 
     41    journal = {Ocean Dynamics}, 
     42    volume = {63}, 
     43    audience = {internationale}, 
     44    doi = {10.1007/S10236-013-0604-6}, 
     45    year = {2013}, 
     46    month = apr, 
     47} 
    548 
    649@inproceedings{AyataLevyEtAl:AMECM:2011, 
     
    39604003  aeresteam = {surf}, 
    39614004  aerestype = {ACL}, 
    3962   comment = {20121123: mauvaise affiliation jb dans hal Contributeur : Francoise 
     4005  comment = {20121123: mauvaise affiliation jb dans hal Contributeur : Françoise 
    39634006        Cudennec <Francoise.Cudennec@ird.fr>}, 
    39644007  doi = {10.1109/TGRS.2012.2188408}, 
     
    79527995 
    79537996@ARTICLE{KurianColasEtAl:JRG:2011, 
    7954   author = {Kurian, Jaison and Colas, Francois and Capet, Xavier and McWilliams, James C. and Chelton, Duddley B.}, 
     7997  author = {Kurian, Jaison and Colas, François and Capet, Xavier and McWilliams, James C. and Chelton, Duddley B.}, 
    79557998  title = {{Eddy properties in the {C}alifornia {C}urrent {S}ystem}}, 
    79567999  journal = {{J}ournal {O}f {G}eophysical {R}esearch {O}ceans}, 
     
    3728337326  number = {1}, 
    3728437327  note = {{I}nter-ocean exchange around southern {A}frica}, 
    37285   comment = {20121114 : mauvaise liste auteur dans doublon hal-00270746 de {F}rancoise 
    37286         {C}udennec <Francoise.Cudennec@ird.fr>}, 
     37328  comment = {20121114 : mauvaise liste auteur dans doublon hal-00270746 de Françoise Cudennec <Francoise.Cudennec@ird.fr>}, 
    3728737329  doi = {10.1016/S0967-0645(02)00396-X}, 
    3728837330  hal_id = {hal-00155070}, 
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