A GENERALIZED EKMAN LAYER PROFILE WITH GRADUALLY VARYING EDDY DIFFUSIVITIES

• The classical analytical solution for the Ekman layer flow has been generalized by introducing an assigned non-rapidly-varying eddy diffusivity K(z). Asymptotic expressions for the wind components u, nu Q obtained via the WKB method retain the form and,

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)

NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

Nyckelord

BOUNDARY-LAYER; BAROCLINIC INSTABILITY; VERTICAL STRUCTURE

Meteorology

Meteorologi

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