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The question posed in the title of this paper is answered in the affirmative by investigating a two-layer, quasi-geostrophic model of the wind-driven circulation. The two layers model the thermocline ...
The stability of the western boundary layer is studied by idealizing it as a parallel flow and solving the OrrSommerfeld equation, generalized to include the gradient of planetary vorticity. The crit...
The structure of a Stommel type of frictional western boundary layer in a thermally driven two-layer model is examined. Instead of specifying the interfacial upwelling a priori, it is calculated as pa...

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