Abstract
A theoretical model of the local circulation in a valley is obtained. The region under study consists of a V-shaped trough of finite length leading into a flat plain, and a given rate of heat flow from ground to air is assumed. The equations of motion are solved numerically, and give a circulation featuring valley and slope winds, their respective anti-winds (compensating flow at higher levels) and vertical currents.
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More From: Archiv für Meteorologie, Geophysik und Bioklimatologie Serie A
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