Polar vortex

Topicupdated 2025-11-22 15:15
Polar vortex

A polar vortex is a large, rotating area of cold air that encircles Earth's polar regions, with distinct stratospheric and tropospheric forms. The stratospheric polar vortex is a high-altitude wind pattern that typically contains extremely cold air over the pole. Its stability is a key factor in influencing winter weather patterns across the Northern Hemisphere.

This phenomenon is notable because when the stratospheric polar vortex weakens or breaks down—an event known as a sudden stratospheric warming—it can have significant downstream effects on weather. During such an event, temperatures in the stratosphere rise dramatically, causing the vortex to slow down, split, or be displaced. This disruption can ultimately allow frigid Arctic air to spill southward, leading to severe cold outbreaks in mid-latitude regions.

Recently, the polar vortex has been in the news due to a significant and unusually timed disruption. Multiple weather reports in November 2025 highlighted the beginning of a rare sudden stratospheric warming event. The magnitude of this event was noted as being almost unprecedented for this early in the winter season.

This development has generated widespread interest because of its potential implications for winter weather. News headlines have generally suggested that such a vortex disruption could lead to a period of intense cold and increased snow potential for parts of North America and Europe, with some reports drawing comparisons to past severe winter events.

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

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