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A Radiative Upper Boundary Condition Adapted for f-Plane Models

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  • 1 National Center for Atmospheric Research, Boulder, CO 80307
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Abstract

Under the assumption of weak background rotational and wind shear effects, an attractive computational upper boundary condition capable of transmitting gravity waves is generalized for use in a variety of f-plane models. Issues relating to numerical implementation are discussed.

Abstract

Under the assumption of weak background rotational and wind shear effects, an attractive computational upper boundary condition capable of transmitting gravity waves is generalized for use in a variety of f-plane models. Issues relating to numerical implementation are discussed.

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