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...
Main Authors: | , , |
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Format: | Text |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | https://doi.org/10.5194/os-2019-114 https://www.ocean-sci-discuss.net/os-2019-114/ |