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...
Main Authors: | Marshall, D, Stephens, J |
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Format: | Journal article |
Language: | English |
Published: |
2001
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