A BAROCLINIC MODEL ATMOSPHERE SUITABLE FOR NUMERICAL INTEGRATION

J. S. Sawyer Meteorological Office, Dunstable

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F. H. Bushby Meteorological Office, Dunstable

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Abstract

Subject to various approximations, a system of three simultaneous partial differential equations is derived to predict the height of a contour surface, the thickness of the layer from 1000 mb to that surface, and the field of vertical velocity averaged throughout a vertical column. The equations are in a form suitable for numerical integration, and a brief outline of a method of solution is given.

Abstract

Subject to various approximations, a system of three simultaneous partial differential equations is derived to predict the height of a contour surface, the thickness of the layer from 1000 mb to that surface, and the field of vertical velocity averaged throughout a vertical column. The equations are in a form suitable for numerical integration, and a brief outline of a method of solution is given.

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