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: M. Le Corre, J. Gula, A.-M. Tréguier
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/os-16-451-2020
https://doaj.org/article/308449237dc34df18e0d593a2a25f3b2