Internal tide generation by seamounts, ridges, and islands

A numerical investigation is made into the generation of semidiurnal internal tides by tidal flow over steep topographic features in the deep ocean. A fully three‐dimensional, free surface, nonlinear, hydrostatic model (the Princeton Ocean Model) is used with real stratification, representative tida...

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Veröffentlicht in:Journal of Geophysical Research, Washington, DC Washington, DC, 1999-11, Vol.104 (C11), p.25937-25951
Hauptverfasser: Holloway, Peter E., Merrifield, Mark A.
Format: Artikel
Sprache:eng
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