Abstract
The circulation in a coastal upwelling region with a shelf area is calculated. It is assumed that the circulation on the shelf is independent of the deep-sea circulation and consists of a surface Ekman layer outflow, a coastal boundary layer upwelling and a bottom Ekman layer inflow. The resultant velocity distribution is used as a boundary condition for the deep-sea circulation....
Recommended Citation
Tomczak, Matthias, and Rolf H. Käse. 1974. "A linear theory of stationary coastal upwelling in a continuously stratified ocean with an unstratified shelf area." Journal of Marine Research 32, (3). https://elischolar.library.yale.edu/journal_of_marine_research/1296
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