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On the Circulation of a Homogeneous Ocean Induced by the Presence of Continental Slopes
Homogeneous Ocean Circulation Presence of Continental
2009/4/2
The three-dimensional circulation of a steady, frictional, homogeneous ocean forced by a wind stress varying sinusoidally in the northward direction is examined, with reference to the effects of conti...
A Model of Tidal Rectification by Potential Vorticity Mixing. Part I: Homogeneous Ocean
Tidal Rectification Potential Vorticity Mixing Homogeneous Ocean
2008/7/10
In previous studies of tidal generation of mean flow over varying topography, the rectification mechanism has generally invoked bottom friction as a source of tidal flux of momentum and vorticity (hen...