The Aleutian Low is a center of atmospheric activity centered over the Aleutian Islands between the east coast of the Siberian Kamchatka Peninsula and the Gulf of Alaska at about 50o N. It is prominent in the winter and disappears in summer, with the average central pressure below 1000 mb in January. This atmospheric activity is a semi-permanent low pressure center. The Aleutian Low is one of the chief centers of action in the atmospheric circulation of the Northern Hemisphere.
|This article is written at a definitional level only. Authors wishing to improve this entry are inivited to expand the present treatment, which additions will be peer reviewed prior to publication of any expansion.|
- Physical Oceanography Index
- J. L. Angell and J. Korshover. Quasi-biennial and long-term fluctuations in the centers of action. Month. Weath. Rev., 102:669 et seq., 1974.