Inviscid equilibria of barotropic flows over finite-amplitude topography are determined by means of statistical mechanics, extending previous quasigeostrophic theory. Imposing constraints of energy and enstrophy conservation leads to a linear relation between equilibrium mean potential vorticity and mean transport streamfunction. This relation is tested numerically and is found to hold over a wide range of topographic amplitudes. Implications for improving parameterizations of entropy generation by eddies are discussed.
机构:
Univ of California, San Diego, CA,, USA, Univ of California, San Diego, CA, USAUniv of California, San Diego, CA,, USA, Univ of California, San Diego, CA, USA
Carnevale, George F.
Frederiksen, Jorgen S.
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机构:
Univ of California, San Diego, CA,, USA, Univ of California, San Diego, CA, USAUniv of California, San Diego, CA,, USA, Univ of California, San Diego, CA, USA