FN Archimer Export Format
PT J
TI Multiscale Observations of Deep Convection in the Northwestern Mediterranean Sea During Winter 2012-2013 Using Multiple Platforms
BT 
AF TESTOR, Pierre
   BOSSE, Anthony
   HOUPERT, Loic
   MARGIRIER, Felix
   MORTIER, Laurent
   LEGOFF, Herve
   DAUSSE, Denis
   LABASTE, Matthieu
   KARSTENSEN, Johannes
   HAYES, Daniel
   OLITA, Antonio
   RIBOTTI, Alberto
   SCHROEDER, Katrin
   CHIGGIATO, Jacopo
   ONKEN, Reiner
   HESLOP, Emma
   MOURRE, Baptiste
   D'ORTENZIO, Fabrizio
   MAYOT, Nicolas
   LAVIGNE, Heloise
   DE FOMMERVAULT, Orens
   COPPOLA, Laurent
   PRIEUR, Louis
   TAILLANDIER, Vincent
   DE MADRON, Xavier Durrieu
   BOURRIN, Francois
   MANY, Gael
   DAMIEN, Pierre
   ESTOURNEL, Claude
   MARSALEIX, Patrick
   TAUPIER-LETAGE, Isabelle
   RAIMBAULT, Patrick
   WALDMAN, Robin
   BOUIN, Marie-Noelle
   GIORDANI, Herve
   CANIAUX, Guy
   SOMOT, Samuel
   DUCROCQ, Veronique
   CONAN, Pascal
AS 1:1;2:2,3;3:4;4:1;5:5;6:1;7:1;8:1;9:6;10:7;11:8;12:8;13:9;14:9;15:10;16:11;17:11;18:12;19:12;20:12;21:12,13;22:12;23:12;24:12;25:14;26:14;27:14;28:15;29:15;30:15;31:16;32:16;33:17;34:17,18;35:17;36:17;37:17;38:17;39:19;
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C1 UPMC Univ Pierre & Marie Curie Paris 06, Sorbonne Univ, CNRS,IRD,MNHN,UMR 7159, Lab Oceanog & Climatol LOCEAN,IPSL,Observ Ecce Te, Paris, France.
   Univ Bergen, Inst Geophys, Bergen, Norway.
   Bjerknes Ctr Climate Res, Bergen, Norway.
   Scottish Assoc Marine Sci, Oban, Argyll, Scotland.
   ENSTA Paristech, Lab Oceanog & Climatol LOCEAN, Palaiseau, France.
   GEOMAR, Kiel, Germany.
   Univ Cyprus, Oceanog Ctr, Nicosia, Cyprus.
   CNR, Ist Ambiente Marino Costiero CNR IAMC Oristano, Oristano, Italy.
   CNR, Ist Sci Marine CNR ISMAR, Venice, Italy.
   Helmholtz Zentrum Geesthacht, Geesthacht, Germany.
   SOCIB, Mallorca, Spain.
   UPMC Univ Pierre & Marie Curie Paris 06, Sorbonne Univ, LOV, Observ Oceanol Villefranche,UMR 7093, Paris, France.
   Ctr Invest Cient & Educ Super Ensenada, Dept Oceanog Fis, Ensenada, Baja California, Mexico.
   Univ Perpignan, CNRS, Ctr Format & Rech Environm Mditerranens CEFREM, Perpignan, France.
   Univ Toulouse, CNRS, Observ Midi Pyrenees, LA, Toulouse, France.
   Univ Toulon & Var, Aix Marseille Univ, CNRS, IRD,MIO,UM 110, Marseille, France.
   Meteo France, CNRS, CNRM, UMR 3589, Toulouse, France.
   IUEM, LOPS, IFREMER, CNRS,IRD,UBO, Plouzane, France.
   UPMC Univ Pierre & Marie Curie Paris 06, Sorbonne Univ, Observ Oceanol Banyuls Mer, Lab Oceanog Microbienne LOMIC,UMR 7093, Paris, France.
C2 CNRS, FRANCE
   UNIV BERGEN, NORWAY
   BCCR, NORWAY
   SAMS SCOTLAND, UK
   ENSTA PARISTECH, FRANCE
   GEOMAR, GERMANY
   UNIV CYPRUS, CYPRUS
   IAMC CNR, ITALY
   IAMC CNR, ITALY
   HZG, GERMANY
   SOCIB, SPAIN
   UNIV PARIS 06, FRANCE
   CICESE, MEXICO
   UNIV PERPIGNAN, FRANCE
   UNIV TOULOUSE, FRANCE
   UNIV TOULON, FRANCE
   CNRM (METEO FRANCE), FRANCE
   UBO, FRANCE
   UNIV PARIS 06, FRANCE
UM LOPS
IF 3.235
TC 65
UR https://archimer.ifremer.fr/doc/00415/52639/53494.pdf
LA English
DT Article
CR DEWEX-MERMEX 2013 LEG1
   DEWEX-MERMEX 2013 LEG2
   DOWEX2012
   DOWEX2013
   HYMEX_SOP1
   HYMEX_SOP2
   MOOSE-GE 2011
   MOOSE-GE 2012
   MOOSE-GE 2013
   MOOSE-GE 2014
   MOOSE-GE 2015
   MOOSE-GE 2016
   MOOSE-GE 2017
BO Le Suroît
   Téthys II
   L'Europe
   L'Atalante
DE ;ocean observation;oceanic deep convection;Mediterranean Sea;energy and buoyancy fluxes;eddies;plumes;symmetric instability
AB During winter 2012-2013, open-ocean deep convection which is a major driver for the thermohaline circulation and ventilation of the ocean, occurred in the Gulf of Lions (Northwestern Mediterranean Sea) and has been thoroughly documented thanks in particular to the deployment of several gliders, Argo profiling floats, several dedicated ship cruises, and a mooring array during a period of about a year. Thanks to these intense observational efforts, we show that deep convection reached the bottom in winter early in February 2013 in a area of maximum 28±3 109m9. We present new quantitative results with estimates of heat and salt content at the sub-basin scale at different time scales (on the seasonal scale to a ten days basis) through optimal interpolation techniques, and robust estimates of the deep water formation rate of 2.0 ± 0.2Sν. We provide an overview of the spatio-temporal coverage that has been reached throughout the seasons this year and we highlight some results based on data analysis and numerical modeling that are presented in this special issue. They concern key circulation features for the deep convection and the subsequent bloom such as Submesoscale Coherent Vortices (SCVs), the plumes and symmetric instability at the edge of the deep convection area. 
PY 2018
PD MAR
SO Journal Of Geophysical Research-oceans
SN 2169-9275
PU Amer Geophysical Union
VL 123
IS 3
UT 000430918500010
BP 1745
EP 1776
DI 10.1002/2016JC012671
ID 52639
ER

EF