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圣塔安那风

维基百科，自由的百科全书
圣安娜风从沙漠中横扫，沿著加利福尼亚南部沿海，将野火焚烧成灰尘和烟雾带到远处太平洋上。 洛杉矶在这张图片的左上方，圣地亚哥靠近中心。

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亚州和北下加利福尼亚半岛。该风经常引起在加州的森林大火。[1][2]

形成

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机制

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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.

另见

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参考资料

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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）. 

外部链接

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