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Examples of katabatic winds include the downslope valley and mountain breezes, the piteraq winds of Greenland, the Bora in the Adriatic, [2] the Bohemian Wind or Böhmwind in the Ore Mountains, the Santa Ana winds in southern California, the oroshi in Japan, or "the Barber" in New Zealand. [3] Not all downslope winds are katabatic.
The Santa Anas are katabatic winds (Greek for "flowing downhill") arising in higher altitudes and blowing down towards sea level. [7] The National Weather Service defines Santa Ana winds as "a weather condition [in southern California] in which strong, hot, dust-bearing winds descend to the Pacific Coast around Los Angeles from inland desert regions".
The Santa Ana winds form in a western area of the country known as the Great Basin, which includes Nevada and part of Utah. The basin sits at a higher elevation than Southern California.
Santa Ana winds (dry downslope winds that affect coastal Southern California and northern Baja California) Santa Lucia winds (a downslope wind affecting southern San Luis Obispo and northern Santa Barbara Counties, California) [citation needed] Squamish (strong, violent wind occurring in many of the fjords of British Columbia)
These notorious and dangerous downslope winds, which occur when higher-level winds are forced over the coastal mountains and toward the coast, typically plague coastal Southern California a few ...
"Chinook" is used for coastal Chinook winds in British Columbia, and is the original use of the term, being rooted in the lore of coastal natives and immigrants, and brought to Alberta by French-speaking fur-traders. [1] [9] Such winds are extremely wet and warm and arrive off the western coast of North America from the southwest.
Santa Ana winds, which gain speed as they blow west and downslope from the Great Basin, are typical at this time of year. But conditions are not normally bone-dry when the winds gust through the ...
A Foehn, or Föhn (UK: / f ɜː n /, US: / f eɪ n / fayn, [2] [3] US also / f ʌ n, f ɜːr n / fu(r)n [4] [5]), is a type of dry, relatively warm downslope wind in the lee of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see ...