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The relation of meridional pressure gradients to North Atlantic deep water volume transport in an ocean general circulation model

Author
GRIESEL, Alexa1 ; MAQUEDA, Miguel Angel Morales2
[1] Potsdam Institute for Climate Impact Research, Telegraphenberg, 14473 Potsdam, Germany
[2] Center for Atmosphere Ocean Science, Courant Institute of Mathematical Sciences, New York University, New York, NY, United States
Source

Climate dynamics. 2006, Vol 26, Num 7-8, pp 781-799, 19 p ; ref : 45 ref

CODEN
CLDYEM
ISSN
0930-7575
Scientific domain
Environment; Climatology, meteorology
Publisher
Springer, Berlin / Springer, Heidelberg
Publication country
Germany
Document type
Article
Language
English
Keyword (fr)
Circulation méridienne Circulation océanique Circulation thermohaline Diffusion tourbillonnaire Gradient densité Gradient pression Mers Antarctiques Modèle circulation générale Modèle océan Océan Atlantique Simulation numérique
Keyword (en)
Meridional circulation ocean circulation thermohaline circulation Eddy diffusion Density gradient Pressure gradient Antarctic Seas General circulation models Ocean model Atlantic Ocean digital simulation
Keyword (es)
Circulación meridiana Circulación oceánica Circulación termohalina Difusión vorticial Gradiente densidad Gradiente presión Mares antárticos Modelo oceánico Océano Atlántico Simulación numérica
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02B Physics of the oceans / 001E02B05 Thermohaline structure and circulation. Turbulence and diffusion

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
17752948

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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