WebA foehn results from the ascent of moist air up the windward slopes; as this air climbs, it expands and cools until it becomes saturated with water vapour, after which it cools more slowly because its moisture is condensing as rain or snow, releasing latent heat. By the time it reaches the peaks and stops climbing, the air is quite dry. WebFoehn events are often accompanied by dramatic cloud formations above the mountains, such as towering lenticular clouds and lower-level rotor clouds. This is seen in the photo below revealing...
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About: Föhn cloud
WebFeb 1, 2024 · Marshall et al. find that surface warming in the region of the AP is substantially greater than that higher up in the troposphere, which casts doubt on the theory that … Webfohn of 20 and 21 May 1937, and finally treats in some detail of the local circula-tion during fohn in the light of modern theory. The fohn wind somewhat ... of the latter shows the Wetterhorn with fohn-cloud just above it, assuming much the shape of the peak itself. THE STRUCTURE OF THE HIMALAYAS Mr. Wadia, as a member of the Geological Survey ... WebIn foehn …of clouds known as a foehn wall, which marks the upper limit of precipitation on the windward slopes. As the air makes its leeward descent, it is compressed and warms … german word for magazine