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• W1997518124 abstract "Abstract The angle between the near‐surface and geostrophic wind vector, α 0 , is discussed in the light of existing and improved Ekman theory and, on the other hand, recently obtained numerical results corroborated by some experimental data, both obtained by other researchers. The latter results for weakly stably stratified boundary layers, also based on large‐eddy simulation (LES) data, give an angle that is about α 0 ≈︁ 35°. If the Ekman theory is applied slightly above the horizontal surface z > 0, for almost any gradually varying eddy diffusivity K ( z ), which is more realistic than K = const used at z = 0 in the classic theory, a closer analytic value to α 0 can be provided (32° to 37°) than that in the classic Ekman theory (45°). Alternatively, and without deploying the refined Ekman surface layer theory already suggested here, one may a priori use the previously confirmed result, α 0 ≈︁ 35°, together with any smooth K ( z ) in order to find the corresponding surface layer depth. These results, bridging the gap between the existing theory toward fine numerical and limited experimental data, may aid further analyses of weakly stably stratified boundary layers. The information about the angle α 0 should be considered in NWP, air‐pollution, wind‐energy and climate models; otherwise, many important boundary‐layer features will remain modelled inadequately. Copyright © 2011 Royal Meteorological Society" @default.
• W1997518124 created "2016-06-24" @default.
• W1997518124 creator A5027914368 @default.
• W1997518124 date "2011-04-01" @default.
• W1997518124 modified "2023-10-09" @default.
• W1997518124 title "The angle of the near-surface wind-turning in weakly stable boundary layers" @default.
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• W1997518124 doi "https://doi.org/10.1002/qj.789" @default.
• W1997518124 hasPublicationYear "2011" @default.
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