Polar vortex

Topicupdated 2025-11-22 13:03
Polar vortex

A polar vortex is a large-scale circulation of cold, rotating air that persistently surrounds Earth's polar regions. It exists in two main forms: the stratospheric polar vortex, high in the atmosphere, and the tropospheric polar vortex, which is closer to the Earth's surface. Both rotate in the same direction as the planet and are fundamental features of the global climate system.

This phenomenon is notable because its behavior directly influences weather patterns across the mid-latitudes, including North America and Europe. When the polar vortex is strong and stable, it tends to confine the coldest air to the Arctic. However, when it weakens or becomes disrupted, it can send frigid air southward, leading to severe cold outbreaks and winter storms far from the poles.

Recently, the polar vortex has been a prominent topic in weather news due to forecasts of a potential weakening event. Multiple major news outlets have reported that a significant disruption to the vortex is anticipated in the late November to early December period. This has led to forecasts suggesting that a surge of unusually cold temperatures could impact parts of the United States following the Thanksgiving holiday, potentially leading to a frigid start to the meteorological winter.

Understanding the dynamics of the polar vortex provides crucial insights for seasonal forecasting. While a weakening event increases the probability of cold air outbreaks, the specific impacts on regional weather are complex and depend on other atmospheric factors, making it a key area of focus for meteorologists.

Brief generated by an LLM (DeepSeek) from Wikipedia and recent news headlines.

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