Response of the bottom boundary layer over a sloping shelf to variations in alongshore wind
Rapidly repeated transects of currents, density, and turbulence through the bottom boundary layer across a relatively uniform stretch of the continental shelf off Oregon reveal the response to a sequence of strong upwelling followed by relaxation and thence a resumption of upwelling. Several definit...
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Veröffentlicht in: | Journal of Geophysical Research. C. Oceans 2005-10, Vol.110 (C10), p.n/a |
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Format: | Artikel |
Sprache: | eng |
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