作者: Roland Meister
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摘要: On the Weissfluhjoch (2690 m a.s.l.) spectrum of horizontal wind speed shows two peaks at frequencies 0.1 and 300 cycles per hour. Vertical profiles in lowest 5 above a crest differs from logarithmical shape. An additional function is fitted to observed deviations can be explained relation with slope angle, surface direction. Drift density are compared free field precipitation rate. Systemes de Vent et Transport Neige en Topographie