A barotropic model of the Ekman planetary boundary layer based on the geostrophic momentum approximation

Details A barotropic model of the Ekman planetary boundary layer based on the geostrophic momentum approximation A barotropic model of the Ekman planetary boundary layer based on the geostrophic momentum approximation

Sep 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987bolme..40..339p&link_type=abstract

Boundary-Layer Meteorology, Volume 40, Issue 4, pp.339-347

Computer Science

4

Scientific paper

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 the top of the boundary layer are derived and analyzed. They underestimate W ∞ compared to the classical expression.

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