An investigation of internal mixing in a seasonally stratified shelf sea

The shelf sea seasonal thermocline is a critical interface within the marine environment, separating the euphotic zone from nutrient‐rich deep water. Fluxes across the thermocline therefore represent a key biogeochemical pathway. In this paper we quantify the rate of mixing across the seasonal therm...

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Veröffentlicht in:Journal of Geophysical Research. C. Oceans 2008-12, Vol.113 (C12), p.n/a
Hauptverfasser: Palmer, Matthew R., Rippeth, Tom P., Simpson, John H.
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Sprache:eng
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