Flow and particle motion induced above a tall seamount by steady and tidal background currents

The response of a stratified ocean over a tall, isolated seamount induced by the combination of slow, steady, spatially uniform inflow and weak diurnal tides is examined using a primitive-equation numerical model. Steady inflow alone forms a Taylor cap, which retains Lagrangian fluid particles over...

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Veröffentlicht in:	Deep-sea research. Part I, Oceanographic research papers Oceanographic research papers, 1997-05, Vol.44 (5), p.719-744
Hauptverfasser:	Goldner, Daniel R., Chapman, David C.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth, ocean, space Exact sciences and technology External geophysics Marine Ocean currents Oceanography Other topics Physics of the oceans Tides
Online-Zugang:	Volltext
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