Eddy shedding from a boundary current around a cape over a sloping bottom
The authors discuss laboratory experiments that elucidate the mechanism of formation and westward drift of anticyclonic baroclinic vortices from a buoyant surface current flowing along a lateral boundary and around a cape. Experiments were carried out with a sloping bottom in order to simulate the t...
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Veröffentlicht in: | Journal of physical oceanography 2000-07, Vol.30 (7), p.1514-1531 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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