Eddy formation on a continental slope
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ID: 304886
1997
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Abstract
We consider a uniform-density ocean in which the depth-independent horizontal velocity is driven by a two-gyre wind. Numerical solutions of the governing vorticity equation reveal that the solutions with a flat ocean bottom differ greatly from those in which a continental shelf and slope are present along the western boundary. In the ocean basin with a western continental shelf, steady inertial circulations readily lose stability to unsteady inertial circulations that spawn eddies. However, eddies do not form in the corresponding solutions for the flat-bottom ocean. Reducing the friction leads to flat-bottom solutions that shed eddies far offshore, but still differ significantly from the corresponding continental-slope solutions, where eddies pinch off near the western boundary.
| Reference Key |
openalex_W2128859440
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|---|---|
| Authors | J. M. Becker, Rick Salmon |
| Journal | journal of marine research |
| Year | 1997 |
| DOI |
10.1357/0022240973224418
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| URL | |
| Keywords | Keywords not found |
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