A nonlinear, three-dimensional model for ocean flows, motivated by some observations of the Pacific Equatorial Undercurrent and thermocline
Using the salient properties of the flow observed in the equatorial Pacific as a guide, an asymptotic procedure is applied to the Euler equation written in a suitable rotating frame. Starting from the single overarching assumption of slow variations in the azimuthal direction in a two-layer, steady...
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Veröffentlicht in: | Physics of fluids (1994) 2017-05, Vol.29 (5) |
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Format: | Artikel |
Sprache: | eng |
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