Fohn wind

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Fohn (Föhn) wind

Fohn (Föhn) windclick for a larger image
Warm and dry winds descending on the leeward side of the mountain. The air falling to the floor of an adjacent valley or plain after blowing across the mountaintop warms up adiabatically. Thus, this wind is warmer than the surrounding air. In Europe, it is known as a Fohn or Föhn wind. In the United States and Canada, along the eastern slopes of the Rockies (i.e., leeward side), the Indian name Chinook is used.
foil
i. A form of metal rolled into a very thin sheet with a thickness less than 0.006 in (0.15 mm).
ii. The spanwise-trailing-edge members forming an integral part of a compound wing.
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In addition, before the cold front arrives, parts of southeastern Taiwan today are likely to see Foehn winds, therefore people are advised to beware of high temperatures.
These are known as Foehn winds, and their warming and drying effect - the Foehn effect - can be striking and farreaching.
The foehn winds coming from the Western Carpathians and reaching the large valleys found in the Tarnave region also have a significant contribution in terms of temperature.
The notoriety of these foehn winds has led to recognition by various local terms: among others, the Chinook and Santa Ana of North America and the Zonda of Argentina.
Traditionally foehn winds are defined as any "warm, dry wind descending in the lee of a mountain range" (Brinkmann 1971, p.
These windstorms are foehn winds, same as the Rocky Mountain chinook (described in IFR, December, 2012) and the same principles apply.
Today a latent poetry echoes in the names we use to distinguish foehn winds from gravity airflows and Katabatic winds from the Khamsin.
The vineyards enjoy a mild continental climate and are exposed to the warm foehn winds.
Shortly thereafter, the forelands and Zurich were caught by surprisingly gusty foehn winds.
The actual, very strong foehn winds touch the surface farther north in the Alpine forelands near Lake Zurich.
Foehn winds occur when strong, deep-layer tropospheric winds blow perpendicular to a mountain range.
The chinook is likely the most severe foehn wind on earth due to the unique physiography and climatology of the Rockies, but what we learn from these chinooks applies equally well to the northeasterly Santa Ana winds of the California coast, the easterly Wasatch winds in the Salt Lake City basin, the east winds of Oregon and Washington, and even the zonda of Argentina.