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foehn

Did you mean: foehn (in meteorology), Foehn (Rock Artist, '90s, 2000s)

 
Dictionary: foehn  föhn (fœn, fān) pronunciation
 
also 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 fœnne, from Old High German phōno, from Vulgar Latin *faōnius, from Latin favōnius, the west wind, from favēre, to be favorable.]


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Word Overheard: foehn
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They go by various names in various parts of the world — chinooks, bergwinds and others — but whatever they're called, the föhns are ill winds indeed:

"Santa Anas are categorized as a föhn wind by meteorologists. The 'murder winds' were termed so during a study by the Ludwig-Maximilians-Universität München in Germany which found a 10 percent increase in suicide and accidents during föhn winds in Central Europe. Santa Anas Winds are of the föhn kind called snow-eaters, because they can swiftly make snow melt in the Alps."

Link: Malibu Arts Reviews Magazine - Malibu Fire Crews Exhausted But Fight On Against The "Devil Winds"

Posted October 28, 2007.

 

When moist air rises over a mountain barrier, it experiences adiabatic temperature changes, and cools at the slow saturated adiabatic lapse rate. Precipitation is common. Once past the mountains, the air, now much drier, descends. It warms at the dry adiabatic lapse rate, higher than the saturated rate by some 3 °C/1000 m. A dry, warm, gusty wind, which can reach gale force, results. Effects in summer can be so desiccating that bush fires are a serious risk; in winter, snow melt can be rapid. See also chinook.

 
foehn (fān, Ger. fön) , warm, dry wind that occurs on the leeward slopes of a ridge of mountains. The term was originally applied to a wind of the Alps but is now used as a generic term for all winds of this type. In other parts of the world the various foehn winds have often been given local names, e.g., the chinook over the eastern slopes of the Rocky Mts., the “sky sweeper” over Majorca, and the aspre over the Garonne plain of France. A foehn originates as follows: Air is first forced upward over the windward mountain slopes, cooling as it encounters the lower pressures of higher altitudes. If, however, it reaches its condensation temperature, the cooling is somewhat reduced owing to the release of latent heat that results from water vapor condensing into liquid water. As the air flows downward over the leeward slopes, it is warmed as it encounters the greater pressures of lower altitudes. This warming, however, is greater than the cooling that occurred during the ascent if heat was added to the air as a result of condensation, so that the air is both warmer and drier than originally. The foehn occurs when the circulation is strong enough to force air over the mountains in a relatively short period of time. The nature of the foehn in a particular locale depends on the topography, the strength and direction of circulation, and the moisture supply on the windward side of the mountains. The chinook, for example, generally blows from the southwest and sometimes raises temperatures by as much as 20°F (7°C) in 15 min.


 
Wikipedia: Foehn wind
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How Foehn is produced
Foehn clouds in Geneva (Switzerland)

A foehn wind or föhn wind is a type of dry down slope wind which occurs in the lee of a mountain range. It is a rain shadow wind which results from the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Föhn winds can raise temperatures by as much as 30°C (86°F)[citation needed] in just a matter of hours. Central Europe enjoys a warmer climate due to the Föhn.

Contents

Effects

Winds of this type are called "snow-eaters" for their ability to make snow melt (also sublimate) rapidly. This snow-removing ability is caused not only by warmer temperatures, but also the low relative humidity of the air mass, having been stripped of moisture by orographic precipitation coming over the mountain(s).

Föhn winds are notorious among mountaineers in the Alps, especially those climbing the Eiger, for whom the winds add further difficulty in ascending an already difficult peak.

They are also associated with the rapid spread of wildfires, making some regions which experience these winds particularly fire-prone.

These winds are often associated with illnesses ranging from migraines to psychosis. A study by the Ludwig-Maximilians-Universität München found that suicide and accidents increased by 10 percent during föhn winds in Central Europe.[citation needed] The causation of Föhnkrankheit (English: Föhn-sickness) is yet unproven. Labelling for preparations of aspirin combined with caffeine, codeine and the like will sometimes include Föhnkrankheit amongst the indications.

Etymology

The name föhn (from the German Föhn, pronounced [ˈføːn]) originated in the alpine region. From Latin (ventus) favonius, a mild west wind of which Favonius was the Roman personification.[1]

Local examples

Regionally, these winds are known by many different names. These include:

The Santa Ana winds of southern California are in some ways similar to the Föhn, but originate in dry deserts as a katabatic wind.

In Popular Culture

Fön trademark

AEG registered the trademark Fön in the 1920s for its hairdryer, which is widely used as a synonym in several languages, such as Finnish, German, Swiss German, Danish, Italian, Dutch, Norwegian, Czech, Croatian, Latvian, Romanian, Slovak, Slovenian, Swedish, Turkish and French in western Switzerland.

See also

References

  • McKnight, TL & Hess, Darrel (2000). Foehn/Chinoonk Winds. In , Physical Geography: A Landscape Appreciation, pp. 132. Upper Saddle River, NJ: Prentice Hall. ISBN 0130202630

Footnotes

  1. ^ Concise Oxford Dictionary, 10th edition, Oxford University Press, entry föhn.

External links


 
 

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