That ring is the stratospheric polar vortex. It sits in the stratosphere, the layer of the atmosphere above where most weather happens. Each autumn, as the Arctic falls into months of darkness, the air above it cools sharply and the vortex strengthens, with winds normally blowing west to east at well over 100 mph.
A strong, steady vortex acts like a fence around the Arctic’s coldest air. When the vortex weakens or splits, that fence can buckle, and lobes of frigid air can push south toward North America, Europe or Asia.
In late October, the vortex’s winds were close to normal. Within days, they collapsed. Measured at a standard height and latitude, they dropped from about 50 mph to about 12 mph in just over a week, then fell to zero and reversed.
That reversal is the official marker of a major sudden stratospheric warming, a rapid heating of the air high above the pole. These events usually happen from mid-winter to early spring. Before this year, the earliest on record were in late November, in 1968 and 2025. This one came weeks earlier than any of them.
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