foehn wind वाक्य
उदाहरण वाक्य
मोबाइल
- The severe weather in the Alps has been studied since the 18th century; particularly the weather patterns such as the seasonal foehn wind.
- 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.
- 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.
- 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.
- Temperatures average between, although the Brookings effect ( or Chetco effect; similar to a foehn wind ) often brings localized hot weather to the Brookings area.
- 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.
- 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.
- 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.
- 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.
- 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.
- A layer of loess, a rather unstable fine silt deposited by the foehn winds which bluster across the plains, covers the northern and western flanks of the peninsula.
- Wind can change the fire-accelerating effect of slopes to effects such as downslope windstorms ( called Santa Anas, foehn winds, East winds, depending on the geographic location ).
- Adiabatic heating occurs in the Earth's atmosphere when an air mass descends, for example, in a katabatic wind, Foehn wind, or chinook wind flowing downhill over a mountain range.
- Southwesterly winds further warmed by foehn wind can give warm temperatures in narrow Norwegian fjords in winter; Tafjord has recorded 17.9 �C in January and Sunndal 18.9 �C in February.
- On average the warmest winter temperatures occur on the south and west coasts, however, warm temperatures occasionally occur due to a foehn wind warming up downwind after the crossing the mountains.
- Since Krak�w lies near the Tatra Mountains, there are often occurrences of halny blowing ( a foehn wind ), causing temperatures to rise rapidly, and even in winter reach up to.
- If the mountain waves break aloft, they can result in strong warm winds at the ground known as Chinook winds ( in North America ) or Foehn winds ( in Europe ).
- The difference in moist adiabatic lapse rate and the dry rate is the cause of foehn wind phenomenon ( also known as " Chinook winds " in parts of North America ).
- The clouds that manage to pass over the mountain, move hastily downwards creating foehn winds that raise the temperature of the area west of the Sierra, which include the Santa Marta, and Ci�naga.
- The Santa Ana is further complicated by downsloped air, or foehn winds, drying out and warming up in the lee of the Sierra Nevada and coastal ranges, leading to a dangerous wildfire situation.
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