Wind Effects in the North Sea

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  • 1 Geophysical Institut, University of Bergen, N-5014 Bergen-Universitetet, Norway
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Abstract

Observed wind-induced fluxes in the Norwegian Trench and on the shallower North Sea Plateau are strongly coupled insofar as variations in one are associated with corresponding but opposing variations in the other. A simple mathematical model indicates that this coupling is topographically controlled.

Abstract

Observed wind-induced fluxes in the Norwegian Trench and on the shallower North Sea Plateau are strongly coupled insofar as variations in one are associated with corresponding but opposing variations in the other. A simple mathematical model indicates that this coupling is topographically controlled.

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