Thermal asymmetry and cross-valley circulation in a small Alpine valley

Wind observations from a small Alpine valley are used to investigate the problem of cross-valley winds. The observed daytime windfield is a superposition of dynamically and thermally forced cross winds. Prevailing cross winds above the valley result in a recirculation cell above the lee slope. The r...

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Veröffentlicht in:	Boundary-layer meteorology 1986-09, Vol.36 (4), p.371-394
1. Verfasser:	HENNEMUTH, B
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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