( ′fān ′ī·lənd ) (meteorology) An isolated area where the foehn has reached the ground, in contrast to the surrounding area where foehn air has not replaced colder surface air.
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foehn also föhn (fn, fn) n. A warm dry wind coming off the lee slopes of a mountain range, especially off the northern slopes of the Alps. [German Föhn, from Middle High German fnn...
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The Chinook winds are nice warming winds that bring instant spring in the middle of winter or a severely destructive windstorm. ... What Is a Foehn Wind ... Humid Air Is Filled Mostly with
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Foehn wind - Wikipedia, the free encyclopedia
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Effet de foehn - Wikipédia
fr.wikipedia.org/wiki/Effet_de_foehn
C'est le cas du vent de Santa Ana qui transporte de l'air sec de l'intérieur des montagnes et descend vers l'océan Pacifique. Il est en partie un foehn et en partie ... |
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The wind speed increases and the vigourous foehn storm can easily reach gale force. (4) Air temperature on the lee-side is now significantly higher than the ...
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Dec 29, 2011 ... Foehn winds are caused by the subsidence of moist air after passing a high mountain. The air is forced to move upslope when encounters a ...
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questions include the real mechanism or mechanisms for the removal of the cold- air pool, the meandering of the foehn flow within the valley, and the asym- ...
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Foehn winds are strong, dry and warm winds that result from the effects that mountains have on the atmosphere. Air that is forced to rise over a mountain barrier ...
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nonfoehn air could still exceed the temperature of the descending foehn air if the upstream air mass was cold and the downstream conditions were nearly cloud ...
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