foehn , także: föhn

Air mass flows down a mountain range, you get a foehn wind.

This is due to foehn wind from south and south-east.

Both areas are subject to the dry hot Zonda (a kind of foehn wind).

This is the result of the phenomenon of foehn wind.

On the northern side Foehn wind is a frequent meteorological phenomenon.

In the summer, the region is cooler than the Pacific area, though it sometimes experiences extremely hot temperatures because of the foehn wind.

On the leeward side of the mountain, the air flowing downward is known as a foehn wind.

The climate in northern Hamamatsu is much harsher because of foehn winds.

The northwesterly wind in the South Island is a foehn wind.

In summer it is a little less rainy than the Pacific area but sometimes experiences extreme high temperatures due to the foehn wind phenomenon.

It is cold, but is distinguished by the occurrence of foehn winds in the upland areas.

You could still make it, but if the foehn winds come early-and they could-then all the snow will melt fast.

The regions near the Alps of the central and eastern plateau sometimes have temperature rises due to the warm foehn wind.

The climate is generally continental, but is moderated by foehn winds blowing from the mountains.

The present name is derived from Favonio, an Italian name for the foehn wind.

The rather cold winters are, however, broken by occasional warmer periods due to foehn wind from the Karawanken mountains to the south.

The Foehn wind, which plays an important role in the northern alpine valleys, has a limited impact on Zurich.

Warmer and drier weather is experienced in the center of the island because the interior's topography encourages foehn winds.

The severe weather in the Alps has been studied since the 18th century; particularly the weather patterns such as the seasonal foehn wind.

The Nor'wester foehn wind is thus a frequent weather pattern, and annual rainfall is only in the region of 300-400mm.

Also note that retardant is generally ineffective when dropped from air during a foehn wind event where winds are blowing from 45-70 mph.

For example, a foehn wind is a type of down-slope wind which occurs in the downwind side of a mountain range.

The primary runway, 02/20, is oriented near perpendicular to Canterbury's Nor'wester foehn wind.

Taxi trials recommenced but with little success till on 21 December 1915 a Foehn wind blew up during trials.

When the wind blows from inland, the resulting hot dry foehn winds are called the Santa Ana Winds.