Turbulent shear flows over low hills

A general analysis is developed for turbulent shear flows over two‐ and three‐dimensional hills with low‐slopes which allows for a wide range of upwind velocity profiles, such as those caused by wakes of upwind hills, roughness changes, or changes in stratification. In this paper the atmosphere is a...

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Veröffentlicht in:	Quarterly journal of the Royal Meteorological Society 1988-10, Vol.114 (484), p.1435-1470
Hauptverfasser:	Hunt, J. C. R., Leibovich, S., Richards, K. J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Convection, turbulence, diffusion. Boundary layer structure and dynamics Earth, ocean, space Exact sciences and technology External geophysics Meteorology
Online-Zugang:	Volltext
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