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Previous studies of forced, long continental shelf waves on an f-plane have considered motion on the shelf and slope which is driven by an alongshore component of the wind stress, essentially through ...
Barotropic Instability of Long Continental Shelf Waves In a Two-Layer Ocean
free continental shelf waves Two-Layer Ocean Barotropic Instability
2009/1/10
A two-layer model is used to examine the properties of free continental shelf waves in the presence of a mean longshore horizontally sheared barotropic current. We allow for discontinuities in the cur...