Barotropic vorticity balance of the North Atlantic subpolar gyre in an eddy-resolving model

The circulation in the North Atlantic subpolar gyre is complex and strongly influenced by the topography. The gyre dynamics are traditionally understood as the result of a topographic Sverdrup balance, which corresponds to a first-order balance between the planetary vorticity advection, the bottom p...

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Bibliographic Details
Published in:Ocean Science
Main Authors: Le Corre, Mathieu, Gula, Jonathan, Tréguier, Anne-marie
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2020
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00629/74062/73537.pdf
https://archimer.ifremer.fr/doc/00629/74062/73538.pdf
https://doi.org/10.5194/os-16-451-2020
https://archimer.ifremer.fr/doc/00629/74062/