A theoretical model of long Rossby waves in the Southern Ocean and their interaction with bottom topography
An analytical model of long Rossby waves is developed for a continuously-stratified, planetary geostrophic ocean in the presence of arbitrary bottom topography under the assumption that the potential vorticity is a linear function of buoyancy. The remaining dynamics are controlled by equations for m...
Main Author: | Marshall, D |
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Format: | Journal article |
Published: |
MDPI
2016
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