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 is traditionally understood as the result of a topographic Sverdrup balance, which corresponds to a first order balance between the planetary vorticity advection, the bottom pr...

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Bibliographic Details
Main Authors: Corre, Mathieu, Gula, Jonathan, Tréguier, Anne-Marie
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/os-2019-114
https://www.ocean-sci-discuss.net/os-2019-114/