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Siberian high |
Also found in: Wikipedia | 0.01 sec. |
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Siberian high [sī′bir·ē·ən ′hī]
(meteorology) An area of high pressure which forms over Siberia in winter, and which is particularly apparent on mean charts of sea-level pressure; centered near lake Baikal. Also known as Siberian anticyclone. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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