Source: wikibot/aleutian-low
= Aleutian Low
{wiki=Aleutian_Low}
The Aleutian Low is a semi-permanent area of low pressure located in the North Pacific Ocean, particularly near the Aleutian Islands of Alaska. It typically develops during the winter months and is characterized by cooler temperatures and stormy weather. The Aleutian Low plays a significant role in the climate and weather patterns of the Pacific Northwest of the United States and parts of Canada.