Aleutian Low

The Aleutian Low is a semi-permanent low-pressure system located near the Aleutian Islands in the Bering Sea during the Northern Hemisphere winter. It is a climatic feature centered near the Aleutian Islands measured based on mean sea-level pressure. It is one of the largest atmospheric circulation patterns in the Northern Hemisphere and represents one of the "main centers of action in atmospheric circulation."^[1]

^ Rodionov, S.N.; Bond, N.A.; Overland, J.E. (November 2007). "The Aleutian Low, storm tracks, and winter climate variability in the Bering Sea". Deep Sea Research Part II: Topical Studies in Oceanography. 54 (23–26): 2560–2577. Bibcode:2007DSRII..54.2560R. doi:10.1016/j.dsr2.2007.08.002.

[RodinovBondOverland-1] Rodionov, S.N.; Bond, N.A.; Overland, J.E. (November 2007). "The Aleutian Low, storm tracks, and winter climate variability in the Bering Sea". Deep Sea Research Part II: Topical Studies in Oceanography. 54 (23–26): 2560–2577. Bibcode:2007DSRII..54.2560R. doi:10.1016/j.dsr2.2007.08.002.

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