Concept information
Término preferido
Aleutian Low
Definición
- 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." (Adapted from: https://en.wikipedia.org/wiki/Aleutian_Low)
Concepto genérico
En otras lenguas
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francés
URI
http://data.loterre.fr/ark:/67375/QX8-35HM6DVC-Q
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