The severe weather in the Alps has been studied since the 18th century; particularly the weather patterns such as the seasonal foehn wind.
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They also can be formed by winds passing hills or mountains, such as Foehn winds, and in this case they can be very regularly shaped.
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During the next day, its eye became obscured after the mountains of New Caledonia affected Rewa's circulation by creating a hot and dry Foehn wind.
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Occasionally, the Foehn winds cause the temperatures to rise unexpectedly : on 22 January 2012 the daily high reached while on 22 February 2012 it reached.
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Temperatures average between, although the Brookings effect ( or Chetco effect; similar to a foehn wind ) often brings localized hot weather to the Brookings area.
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Also note that retardant is generally ineffective when dropped from air where winds are blowing down a hill ( foehn wind event ) from 45-70 mph.
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The period of windless weather appears interestingly regularly, caused by the cover of, and the dry down-slope foehn winds arriving from, the Beskid Zlski mountain range.
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The Zonda, a Foehn wind characterized by warm, dry air can cause temperatures to exceed in some cases while in summer, temperatures can exceed such as in 2003.
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The prevailing wind in Christchurch is from the north-east and to a lesser extent from the south-west, but the city is also affected by Canterbury's nor'wester foehn wind.
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Prevailing winds blow from W, S, E and NE . Southwesterly winds, known as libeccio or garbino, are foehn winds, which may bring warm temperatures in each season.
