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equivalent barotropic model |
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equivalent barotropic model [i′kwiv·ə·lənt bar·ə′träp·ik ′mäd·əl] (meteorology) A model atmosphere characterized by frictionless and adiabatic flow and by hydrostatic quasigeostrophic equilibrium, and in which the vertical shear of the horizontal wind is assumed to be proportional to the horizontal wind itself. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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