A Vertically Integrated Primitive-Equation Model
نویسنده
چکیده
I ABSTRACT-The primitive equations are integrated with The model includes topography and is capable of respondrespect to the vertical coordinate, sigma. The resulting ing to diabatic heating. Experiments with and without equations contain vertical eddy terms arising from nonthe continuity equation are carried out, and a comparison linearities. These eddies are parameterized using a is made with barotropic forecasts. Exclusion of the mass standard-atmosphere temperature distribution and a continuity condition results in superior forecasts, especially linear jet wind profile independent of horizontal position. I
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