Williwaw

In meteorology, a williwaw is a sudden blast of wind descending from a mountainous coast to the sea. The word is of unknown origin, but was earliest used by British seamen in the 19th century. The usage appears for winds found in the Strait of Magellan, the Aleutian Islands and the coastal fjords of the Alaskan Panhandle, where the terms outflow wind and squamish wind are also used for the same phenomenon. On Greenland the word piteraq is used.

The williwaw results from the descent of cold, dense air from the snow and ice fields of coastal mountains in high latitudes, accelerated by the force of gravity. Thus the williwaw is considered a type of katabatic wind.

In popular culture

See also

References

  1. ^ Winds of the World: The Williwaw, from Weather Online
  2. ^ Mentions Williwaw as an Aleut Word , from The Thousand Mile War
This article is issued from Wikipedia - version of the Friday, March 18, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.