globalchange  > 气候减缓与适应
DOI: 10.1002/2016JC012671
Scopus记录号: 2-s2.0-85042640249
论文题名:
Multiscale Observations of Deep Convection in the Northwestern Mediterranean Sea During Winter 2012–2013 Using Multiple Platforms
作者: Testor P.; Bosse A.; Houpert L.; Margirier F.; Mortier L.; Legoff H.; Dausse D.; Labaste M.; Karstensen J.; Hayes D.; Olita A.; Ribotti A.; Schroeder K.; Chiggiato J.; Onken R.; Heslop E.; Mourre B.; D'ortenzio F.; Mayot N.; Lavigne H.; de Fommervault O.; Coppola L.; Prieur L.; Taillandier V.; Durrieu de Madron X.; Bourrin F.; Many G.; Damien P.; Estournel C.; Marsaleix P.; Taupier-Letage I.; Raimbault P.; Waldman R.; Bouin M.-N.; Giordani H.; Caniaux G.; Somot S.; Ducrocq V.; Conan P.
刊名: Journal of Geophysical Research: Oceans
ISSN: 21699275
出版年: 2018
卷: 123, 期:3
起始页码: 1745
结束页码: 1776
语种: 英语
英文关键词: eddies ; energy and buoyancy fluxes ; Mediterranean Sea ; ocean observation ; oceanic deep convection ; plumes ; symmetric instability
Scopus关键词: buoyancy ; data interpretation ; deep water formation ; deep water ventilation ; eddy ; energy flux ; flux measurement ; interpolation ; numerical model ; oceanic convection ; plume ; thermohaline circulation ; winter ; Gulf of Lion ; Mediterranean Sea ; Mediterranean Sea (Northwest)
英文摘要: 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 109m2. We present new quantitative results with estimates of heat and salt content at the subbasin scale at different time scales (on the seasonal scale to a 10 days basis) through optimal interpolation techniques, and robust estimates of the deep water formation rate of 2.0±0.2 Sv. We provide an overview of the spatiotemporal 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. © 2017. American Geophysical Union. All Rights Reserved.
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/114420
Appears in Collections:气候减缓与适应

Files in This Item:

There are no files associated with this item.


作者单位: CNRS-Sorbonne Universités (UPMC Univ. Pierre et Marie Curie, Paris 06)-CNRS-IRD-MNHN, UMR 7159, Laboratoire d'Océanographie et de Climatologie (LOCEAN), Institut Pierre Simon Laplace (IPSL), Observatoire Ecce Terra, Paris, France; Geophysical Institute, University of Bergen and Bjerknes Center for Climate Research, Bergen, Norway; Scottish Association for Marine Science, Oban, Argyll, United Kingdom; ENSTA–Paristech, Laboratoire d'Océanographie et de Climatologie (LOCEAN), Palaiseau, France; GEOMAR, Kiel, Germany; Oceanography Center, University of Cyprus, Nicosia, Cyprus; Consiglio Nazionale delle Ricerche - Istituto per l'ambiente Marino Costiero (CNR-IAMC) Oristano, Oristano, Italy; Consiglio Nazionale delle Ricerche - Istituto di Scienze Marine (CNR-ISMAR), Venezia, Italy; Helmholtz-Zentrum Geesthacht, Geesthacht, Germany; SOCIB, Mallorca, Spain; Sorbonne Universités (UPMC Univ. Pierre et Marie Curie, Paris 06), UMR 7093, Laboratoire d'Océanographie de Villefranche (LOV), Observatoire Océanologique de Villefranche/mer, France; Departamento de Oceanografa Fisica, Centro de Investigacion Cientfica y de Educacion Superior de Ensenada, Ensenada, Baja California, Mexico; CNRS-Université de Perpignan, Centre de Formation et de Recherche sur les Environnements Mditerranens (CEFREM), Perpignan, France; CNRS-Universit de Toulouse, Laboratoire d'Aerologie (LA), Observatoire Midi-Pyrénées, Toulouse, France; Aix-Marseille Université, Université de Toulon, CNRS, IRD, MIO UM 110, Marseille, France; MétéoFrance/CNRS, CNRM, UMR 3589, Toulouse, France; Ifremer-CNRS-IRD-UBO, LOPS, IUEM, Plouzané, France; Sorbonne Universités (UPMC Univ. Pierre et Marie Curie, Paris 06), UMR 7093, Laboratoire d'Océanographie Microbienne (LOMIC), Observatoire Océanologique de Banyuls/mer, France

Recommended Citation:
Testor P.,Bosse A.,Houpert L.,et al. Multiscale Observations of Deep Convection in the Northwestern Mediterranean Sea During Winter 2012–2013 Using Multiple Platforms[J]. Journal of Geophysical Research: Oceans,2018-01-01,123(3)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Testor P.]'s Articles
[Bosse A.]'s Articles
[Houpert L.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Testor P.]'s Articles
[Bosse A.]'s Articles
[Houpert L.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Testor P.]‘s Articles
[Bosse A.]‘s Articles
[Houpert L.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.