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Siberian high

   Also found in: Wikipedia 0.01 sec.
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.


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15 GEOPHYSICAL RESEARCH LETTERS, scientists report that the strength of the Siberian high is linked to the amount of early-season snow cover in this Russian region.
 
 
 
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