On the insensitivity of the wind-driven circulation to bottom topography

An analytical model is developed for the wind-driven circulation in a continuously stratified ocean overlying variable bottom topography. In the ocean interior we adopt a linear relation between potential vorticity, density and Montgomery potential, resulting in Welander's solution for an adiab...

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Bibliographic Details
Main Authors: Marshall, D, Stephens, J
Format: Journal article
Language:English
Published: 2001

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