Abstract
The generalized Ekman equation is often that the vertical variation of both the eddy diffusivity used for micrometeorological applications. Use of the and the thermal wind is important to the determination , noniterative numerical technique of superposition reveals of the wind profile when this equation is applicable.
Cite
CITATION STYLE
APA
SCHAEFER, J. T. (1973). On the Solution of the Generalized Ekman Equation. Monthly Weather Review, 101(6), 535–537. https://doi.org/10.1175/1520-0493(1973)101<0535:otsotg>2.3.co;2
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