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聖塔安那風

维基百科，自由的百科全书
聖安娜風從沙漠中橫掃，沿著加利福尼亞南部沿海，將野火焚燒成灰塵和煙霧帶到遠處太平洋上。 洛杉磯在這張圖片的左上方，聖地亞哥靠近中心。

圣塔安娜风是一种典型的南加州季节性强风。圣塔安娜风是强烈且非常干燥的下坡风，起源于内陆，影响到沿海的南加利福尼亞州和北下加利福尼亚半岛。該風經常引起在加州的森林大火。[1][2]

形成

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機制

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This map illustration shows a characteristic high-pressure area centered over the Great Basin, with the clockwise anticyclone wind flow out of the high-pressure center giving rise to a Santa Ana wind event as the airmass flows through the passes and canyons of southern California, manifesting as a dry northeasterly wind.

另見

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參考資料

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  1. ^ Masters, Nathan. SoCal's Devil Winds: The Santa Anas in Historical Photos and Literature. www.kcet.org. KCET. October 25, 2012 [May 3, 2012]. （原始内容存档于October 29, 2012）.  "(White)Scholars who have looked into the name's origins generally agree that it derives from Santa Ana Canyon, the portal where the Santa Ana River -- as well as a congested Riverside (CA-91) Freeway -- leaves Riverside County and enters Orange County. When the Santa Anas blow, winds can reach exceptional speeds in this narrow gap between the Puente Hills and Santa Ana Mountains."
  2. ^ Needham, John. The Devil Winds Made Me Do It : Santa Anas Are Enough to Make Anyone's Hair Stand on End. www.latimes.com. Los Angeles Times. March 12, 1988 [May 3, 2013]. （原始内容存档于April 29, 2014）. 

外部連結

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