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Foehn wind

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Isentropic draw-down is the draw-down of warmer, drier air from aloft. When the approaching winds are insufficiently strong to propel the low-level air up and over the mountain barrier, the airflow is said to be 'blocked' by the mountain and only air higher up near mountain-top level is able to pass
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When winds blow over elevated terrain, air forced upwards expands and cools due to the decrease in pressure with height. Since colder air can hold less water vapour, moisture condenses to form clouds and precipitates as rain or snow on the mountain's upwind slopes. The change of state from vapour to
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Dry Foehn conditions are responsible for the occurrence of rain shadows in the lee of mountains, where clear, sunny conditions prevail. This often leads to greater daytime radiative (solar) warming under Foehn conditions. This type of warming is particularly important in cold regions where snow or
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In some regions, Foehn winds are associated with causing circulatory problems, headaches, or similar ailments. Researchers have found, however, the Foehn wind's warm temperature to be beneficial to humans in most situations, and have theorised that the reported negative effects may be a result of
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When river water passes over rocks, turbulence is generated in the form of rapids, and white water reveals the turbulent mixing of the water with the air above. Similarly, as air passes over mountains, turbulence occurs and the atmosphere is mixed in the vertical. This mixing generally leads to a
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energy which heats the air, partially countering the cooling that occurs as the air rises. The subsequent removal of moisture as precipitation renders this heat gain by the air irreversible, leading to the warm, dry, Foehn conditions as the air descends in the mountain's lee. This mechanism has
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There are four known causes of the Foehn warming and drying effect. These mechanisms often act together, with their contributions varying depending on the size and shape of the mountain barrier and on the meteorological conditions, such as the upstream wind speed, temperature and humidity.
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secondary factors, such as changes in the electrical field or in the ion state of the atmosphere, the wind's relatively low humidity, or the generally unpleasant sensation of being in an environment with strong and gusty winds.
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over and down the lee slopes as Foehn winds. These higher source regions provide Foehn air that becomes warmer and drier on the leeside after it is compressed with descent due to the increase in pressure towards the surface.
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become a popular textbook example of atmospheric thermodynamics. However, the common occurrence of 'dry' Foehn events, where there is no precipitation, implies there must be other mechanisms.
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by as much as 14 °C (25 °F) in just a matter of hours. Switzerland, southern Germany, and Austria have a warmer climate due to the Foehn, as moist winds off the
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downward warming and upward moistening of the cross-mountain airflow, and consequently to warmer, drier Foehn winds in the valleys downwind.
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was originally used to refer to the south wind which blows during the winter months and brings thaw conditions to the northern side of the
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Elevated fire danger conditions associated with foehn-like winds in southeastern Australia. Journal of Applied Meteorology and Climatology
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on account of its extremely hot weather in summer resulting from the adiabatic warming effect created by mountains further south.
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Rotor cloud revealing overturning and turbulence above the lee slopes of the Antarctic Peninsula during a westerly Foehn event
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side, loses much of its water vapour content, and descends on the French plateau and valley of the Mont-Cenis range in the
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See the documentary: Snow Eater (the English translation of Canadian First Nations word phonetically pronounced chinook).
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Anecdotally, residents in areas of frequent Foehn winds have reported experiencing a variety of illnesses ranging from
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Tuller, Stanton E. (April 1980). "The Effects of a Foehn Wind on Human Thermal Exchange: The Canterbury Nor'wester".
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Giannini, AJ; Malone, DA; Piotrowski, TA (1986). "The serotonin irritation syndrome – a new clinical entity?".
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Elvidge, Andrew D.; Renfrew, Ian A.; King, John C.; Orr, Andrew; Lachlan-Cope, Tom A. (January 2016).
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in the Hakkâri Province, which are roughly on the same latitude but are on the windward side of the
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Romanić; et al. (2015). "Long-term trends of the 'Koshava' wind during the period 1949–2010".
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wind, causing warm temperatures in the leeward side of mountains in the mild-winter climate of the
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winds of Santa Barbara, are in some ways similar to the Föhn, but originate in dry deserts as a
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Winds of this type are also called "snow-eaters" for their ability to make snow and ice melt or
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and accidents increased by 10 percent during Foehn winds in Central Europe. The causation of
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rapidly. This is a result not only of the warmth of Foehn air, but also its low relative
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Foehn winds are notorious among mountaineers in the Alps, especially those climbing the
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Foehn can be initiated when deep low-pressure systems move into Europe, drawing moist
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Romanić; et al. (2015). "Contributing factors to Koshava wind characteristics".
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of moist and dry air, the air on the leeward slopes becomes warmer than equivalent
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The strong clouds at the mountain ridges where the Föhn winds form are called
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Regionally, these winds are known by many different names. These include:
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The causes of the Foehn effect in the lee of mountains (adapted from: )
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on the southwestern coast of Oregon, also known as the Chetco Effect.
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McKnight, TL & Hess, Darrel (2000). "Foehn/Chinook Winds". In
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in the United States and Canada, and north, east and west of the
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Viento del Sur (Southern Wind) or Hego haizea in Basque in the
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Sharples, J.J. Mills, G.A., McRae, R.H.D., Weber, R.O. (2010)
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The Routledge Dictionary of Pronunciation for Current English
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10.1175/1520-0434(2002)017<0907:UWIBFW>2.0.CO;2
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Dissolving clouds from Foehn wind over the Cumbre Nueva in
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was the Roman personification and probably transmitted by
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The warm moist air from northern Italy is blocked on the
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warming of air that has dropped most of its moisture on
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ice melt is a concern or where avalanches are a risk.
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Quarterly Journal of the Royal Meteorological Society
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Mountains and their respective leeward valleys, the
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Type of dry down-slope wind occurring near mountains
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Foehn chart provided by meteomedia/meteocentrale.ch
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Cambridge University Press. 690:Foehn winds in the foothills of the southern 265: 1373:Physical Geography: A Landscape Appreciation 1046:Föhn or Foehn in Austria, southern Germany, 356: 342: 313: 307: 279: 2048:Movie of a Föhn situation in the Swiss Alps 810: 247: 1879: 1822: 1757: 1755: 1679: 1580:. February 8, 2006. See January 22 entry. 1429: 924:in China is famously known as one of the 631:Learn how and when to remove this message 489:Learn how and when to remove this message 2053:East Scotland warmth due to Foehn Effect 1625: 1463:Cambridge English Pronouncing Dictionary 1258:Foehn over Carretera Punta de Jandía in 1012:due to south-western winds crossing the 975: 959: 851:In winter, a Foehn effect occurs in the 402: 368: 33: 25: 1955: 1912: 411: 2072: 1761: 1752: 1563: 1518:; Kretzschmar, William A. Jr. (2017). 541:Ludwig-Maximilians-Universität München 178:wind that results from the subsequent 1486: 1444: 237: 162:), is a type of dry, relatively warm 1958:International Journal of Climatology 1915:International Journal of Climatology 829: 613:adding citations to reliable sources 584: 561:and the like will sometimes include 471:adding citations to reliable sources 442: 429: 420: 332:French-speaking parts of Switzerland 821: 13: 1784:10.1111/j.1745-7939.1980.tb01919.x 1697:The Journal of Clinical Psychiatry 14: 2111: 2026: 580: 1632:Der Brockhaus. Wetter und Klima. 1492:Longman Pronunciation Dictionary 1303: 1291: 1275: 1251: 1068:in Finland as moist air crosses 589: 447: 127: 96: 70: 2005: 1992: 1949: 1906: 1888: 1847: 1790: 1735: 1715: 1688: 1644: 600:needs additional citations for 527:Purported physiological effects 458:needs additional citations for 246:region. Originating from Latin 1600: 1584: 1549:Merriam-Webster.com Dictionary 1536: 1508: 1480: 1438: 390:Condensation and precipitation 1: 2019:. Retrieved 17 February 2018. 1365: 1387: 252:, a mild west wind of which 216: 7: 1522:(2nd ed.). Routledge. 1323: 1016:(mostly in fall and winter) 809:Garmesh, Garmij, Garmbaad ( 10: 2116: 1298:Foehn over Llano del Jable 1244: 1158:, and most notoriously in 947:) in northern and central 438: 270:, the term was adopted as 18: 2013:The Canterbury nor'wester 1591:Concise Oxford Dictionary 1494:(3rd ed.). Longman. 1431:10.1175/bams-d-14-00194.1 1019:Fen in northwest Slovenia 768:Newfoundland and Labrador 364: 198:on the windward slopes. 1854:David M. Gaffin (2002). 1797:David M. Gaffin (2007). 1747:University of Canterbury 1575:National Weather Service 887:in Iraqi Kurdistan, and 853:West Azerbaijan province 687:of Alaska, United States 1860:Weather and Forecasting 1803:Weather and Forecasting 1650: 1578:Weather Forecast Office 1111:Hnjúkaþeyr in Icelandic 840:) in the south west of 275: 2017:New Zealand Geographic 1764:New Zealand Geographer 1403: 1213:, and also in eastern 1070:Scandinavian Mountains 985: 973: 964:Foehn clouds upon the 944: 939:), hot-dry west wind ( 936: 408: 395:liquid water releases 382: 357: 343: 314: 308: 294: 289: 280: 266: 261: 248: 230: 201:Foehn winds can raise 51: 31: 1743:Grumpy nor'west winds 979: 963: 745:on the west coast of 692:Appalachian Mountains 406: 372: 320:genericized trademark 170:(downwind side) of a 37: 29: 2085:Mountain meteorology 1203:Great Dividing Range 1195:Great Dividing foehn 1080:Carpathian Mountains 609:improve this article 467:improve this article 412:Isentropic draw-down 1970:2015IJCli..35..288R 1927:2016IJCli..36..956R 1872:2002WtFor..17..907G 1815:2007WtFor..22..145G 1776:1980NZGeo..36...11T 1672:2016QJRMS.142..618E 1422:2016BAMS...97..455E 903:Indo-Gangetic Plain 879:is much lower than 723:San Fernando Valley 166:that occurs in the 2090:Weather and health 2063:2013-04-03 at the 2033:Photo of Föhnmauer 1728:2013-10-17 at the 1205:, observed in the 1014:Apennine Mountains 1001:(mostly in winter) 993:and north-western 986: 980:Foehn clouds over 974: 877:Iranian Azerbaijan 747:Cape Breton Island 409: 383: 306:. 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Retrieved 1614:. 2009-01-22 1611: 1602: 1594: 1590: 1586: 1565: 1554:. Retrieved 1547: 1538: 1519: 1516:Upton, Clive 1510: 1491: 1482: 1461: 1458:Esling, John 1454:Setter, Jane 1450:Roach, Peter 1440: 1413: 1409: 1372: 1340:Chinook wind 1217:and eastern 1125:and western 1064:and Western 1062:Ostrobothnia 1024:South Norway 918:, Indonesia. 794:Signy Island 764:Newfoundland 737:Puelche wind 715:Santa Monica 701:of southern 675:east of the 642: 627: 618: 607:Please help 602:verification 599: 575: 562: 548: 530: 518: 511: 500: 485: 476: 465:Please help 460:verification 457: 433: 424: 415: 393: 384: 340: 327: 222: 220: 203:temperatures 200: 186:slopes (see 59: 55: 53: 44:Cumbre Nueva 2080:Föhn effect 2011:Relph, D. 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Index

Henschel Hs 297


Föhn clouds
Cumbre Nueva
La Palma
UK
/fɜːn/
US
/fn/
fayn
US
/fʌn,fɜːrn/
fu(r)n
downslope wind
lee
mountain range
rain shadow
adiabatic
windward
orographic lift
lapse rates
elevations
temperatures
Mediterranean Sea
Alps
German
[ˈføːn]
Alpine
Favonius

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