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Topographic stress parameterization in a quasi-geostrophic barotropic model
Published online by Cambridge University Press: 25 June 1997
Abstract
The physical basis for parameterizing topographic stress due to unresolved eddies is examined in a quasi-geostrophic barotropic model. Topographic stress parameterization is shown to represent two effects of eddies: attraction of the flow to a statistical equilibrium featuring topographically correlated mean currents, and dissipation of potential enstrophy. Performance is evaluated by comparing parameterized low-resolution models with explicit high-resolution models.
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- © 1997 Cambridge University Press
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