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In most of this region, there is extremely limited precipitation during the winter, owing to the powerful anticyclonic winds from Siberia.
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The direction an eddy swirls can be categorized as either cyclonic or anticyclonic depending on the hemisphere.
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The low, sharp inversion can lead to areas of persistent stratocumulus or stratus cloud, colloquially known as anticyclonic gloom.
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The low, sharp temperature inversion can lead to areas of persistent stratocumulus or stratus cloud, known in colloquial terms as anticyclonic gloom.
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Such tornadoes are more often anticyclonic than are typical tornadoes and these pairs may be referred to as tornado couplets.
en.wikipedia.org
Flow over the shelf below the surface layer consists of two anticyclonic gyres connected by a central cyclonic flow.
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