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
Hauptverfasser: Perlin, A., Moum, J. N., Klymak, J. M.
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Sprache:eng
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