Other
Scientific paper
Jul 1983
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983bolme..26..209m&link_type=abstract
Boundary-Layer Meteorology, Volume 26, Issue 3, pp.209-226
Other
3
Scientific paper
The equations of motions are solved for concentric circular flow in the planetary boundary layer (PBL) under the assumption of K = l 2|∂v/∂z| and gradient wind independent of radius r. The theoretical distribution of wind is obtained for r ≥ 300 km. Other parameters of the PBL are also calculated. Finally, equilibrium of the forces in the PBL is analyzed.
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