What is the name of the low-pressure cell associated with the Polar Front?

The Aleutian Low is indeed the name of the low-pressure cell that is associated with the Polar Front. This significant weather system occurs in the North Pacific Ocean, particularly between the Aleutian Islands and the Bering Sea, where cold polar air meets warmer air from the ocean. This interaction creates the conditions necessary for the formation of a low-pressure system characterized by cloudy weather, precipitation, and often stormy conditions.

The Aleutian Low plays a critical role in the climate and weather patterns of the region, directly impacting the surrounding ecosystems and influencing atmospheric circulation. It is essential to understand these dynamics, as they help explain various weather phenomena experienced in coastal Alaska and the broader North Pacific area. While the Gulf Stream and the Icelandic Low are also relevant climatic features, they do not specifically pertain to the Polar Front in the same direct manner as the Aleutian Low.