A barotropic model of the Ekman planetar
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S. Panchev; T. S. Spassova
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Article
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1987
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Springer
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English
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A model of a stationary planetary boundary layer is proposed based on the equation of motion with the advective term retained. The latter is modeled by means of the so-called geostrophic momentum approximation in two versions -original and modified. New expressions for the vertical velocity W, at th