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The demonstration that three foehn warming mechanisms are important has ramifications for weather forecasting in mountainous areas and associated hazards such as ice shelf melt and wildfires.
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Föhn (the name is also spelled as Fohn, Foehn and Föhnwind) is another mountain wind. It blows from the mountains to the valley and brings very dry and very warm air. This wind occurs in many mountainous areas of the world: in the Alps, in the mountains of Central Asia, in the Caucasus, in the Rocky Mountains of North America and other places.
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The mean foehn duration over all foehn events based on 10-min resolution data were around 7.5 h. Therefore, the upscaling of the Duerr index to 6-hourly resolution allows us to capture most foehn events, which is further underlined by the similar foehn occurrence in both datasets (cf. Table 1 ).
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Foehn winds are warm, dry downslope winds that occur on the lee side of topographic barriers. In southwestern Alberta, Canada, wind erosion is periodically associated with strong foehn winds that flow down the eastern flank of the Rocky Mountains, locally known as Chinooks.. (1−1.5 km above the sea level). The snowpacks reach the annual.
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foehn, warm and dry, gusty wind that periodically descends the leeward slopes of nearly all mountains and mountain ranges. The name was first applied to a wind of this kind that occurs in the Alps, where the phenomenon was first studied. A foehn results from the ascent of moist air up the windward slopes; as this air climbs, it expands and.
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The particular term föhn is associated with the Alps. When moist air is forced to rise over the mountains, it cools at the saturated adiabatic lapse-rate (0.5°C·100 m −1). The humidity increases until the condensation begins. Precipitation may occur and föhn clouds can be formed. Föhn clouds are either orographic clouds or mountain wave.
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The rate of temperature variation for the dry air (dry adiabatic lapse rate) is around 10°C /km (around 5.5 °F per 1,000 ft) and of around 6°C / km (around 3.3°F per 1,000 ft) for saturated air (moist adiabatic lapse rate). The Foehn effect don't always produce rain, snow or even thick clouds on the upwind side. When there is no.
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A Foehn or Föhn ( UK: / fɜːn /, US: / feɪn /, [2] [3] US also / fʌn, fɜːrn / [4] [5] ), is a type of dry, relatively warm, downslope wind that occurs in the lee (downwind side) of a mountain range.