How the polar vortex and heat ocean are intensifying a significant US winter storm

A extreme winter storm sweeping throughout the central and jap U.S. in late January 2026 threatened states from Texas to New England with crippling freezing rain, sleet and snow. A number of governors issued states of emergency as forecasters warned of hazardous journey situations, harmful wind chills and energy outages amid bitter chilly anticipated to linger for days.

The sudden blast could come as a shock to many People after a mostly mild start to winter, however that heat could also be partly contributing to the ferocity of this storm.

As atmospheric and climate scientists, we conduct analysis that goals to enhance understanding of utmost climate, together with what makes it roughly more likely to happen and the way local weather change may or may not play a job.

To know what People are experiencing with this winter blast, we have to look greater than 20 miles above the floor of Earth, to the stratospheric polar vortex.

A forecast for Jan. 26, 2026, reveals the freezing line in white reaching far into Texas. The sunshine band with arrows signifies the jet stream, and the darkish band signifies the stratospheric polar vortex. The jet stream is proven at about 3.5 miles above the floor, a typical top for monitoring storm programs. The polar vortex is roughly 20 miles above the floor.
Mathew Barlow, CC BY

What creates a extreme winter storm like this?

A number of climate components have to return collectively to supply such a big and extreme storm.

Winter storms sometimes develop the place there are sharp temperature contrasts close to the floor and a southward dip in the jet stream, the slim band of fast-moving air that steers climate programs. If there’s a substantial supply of moisture, the storms can produce heavy rain or snow.

In late January, a powerful Arctic air mass from the north was creating the temperature distinction with hotter air from the south. A number of disturbances inside the jet stream had been performing collectively to create favorable situations for precipitation, and the storm system was capable of pull moisture from the very warm Gulf of Mexico.

A map of storm warnings on Jan. 24, 2026.

The Nationwide Climate Service issued extreme storm warnings (pink) on Jan. 24, 2026, for a big swath of the U.S. that would see sleet and heavy snow over the next days, together with ice storm warnings (darkish purple) in a number of states and excessive chilly warnings (darkish blue).
National Weather Service

The place does the polar vortex are available in?

The quickest winds of the jet stream happen just under the highest of the troposphere, which is the bottom degree of the ambiance and ends about seven miles above Earth’s floor. Climate programs are capped on the high of the troposphere, as a result of the ambiance above it turns into very steady.

The stratosphere is the subsequent layer up, from about seven miles to about 30 miles. Whereas the stratosphere extends excessive above climate programs, it will probably nonetheless work together with them by way of atmospheric waves that transfer up and down within the ambiance. These waves are much like the waves within the jet stream that trigger it to dip southward, however they transfer vertically as a substitute of horizontally.

A chart reveals how temperatures within the decrease layers of the ambiance change between the troposphere and stratosphere. Miles are on the suitable, kilometers on the left.
NOAA

You’ve most likely heard the time period “polar vortex” used when an space of chilly Arctic air strikes far sufficient southward to affect the USA. That time period describes air circulating across the pole, however it will probably discuss with two different circulations, one within the troposphere and one within the stratosphere.

The Northern Hemisphere stratospheric polar vortex is a belt of fast-moving air circulating across the North Pole. It is sort of a second jet stream, excessive above the one you might be conversant in from climate graphics, and often much less wavy and nearer to the pole.

Generally the stratospheric polar vortex can stretch southward over the USA. When that occurs, it creates very best situations for the up-and-down motion of waves that connect the stratosphere with severe winter weather on the floor.

A stretched stratospheric polar vortex displays upward waves again down, left, which impacts the jet stream and floor climate, proper.
Mathew Barlow and Judah Cohen, CC BY

The forecast for the January storm confirmed an in depth overlap between the southward stretch of the stratospheric polar vortex and the jet stream over the U.S., indicating excellent situations for chilly and snow.

The most important swings in the jet stream are related to essentially the most vitality. Below the suitable situations, that vitality can bounce off the polar vortex back down into the troposphere, exaggerating the north-south swings of the jet stream throughout North America and making extreme winter climate extra probably.

That is what was occurring in late January 2026 within the central and jap U.S.

If the local weather is warming, why are we nonetheless getting extreme winter storms?

Earth is unequivocally warming as human actions launch greenhouse gasoline emissions that entice warmth within the ambiance, and snow amounts are decreasing overall. However that doesn’t imply extreme winter climate won’t ever occur once more.

Some analysis means that even in a warming setting, chilly occasions, whereas occurring much less incessantly, may still remain relatively severe in some locations.

One issue could also be increasing disruptions to the stratospheric polar vortex, which look like linked to the rapid warming of the Arctic with local weather change.

Two globes, one showing a stable polar vortex and the other a disrupted version that brings brutal cold to the South.

The polar vortex is a powerful band of winds within the stratosphere, usually ringing the North Pole. When it weakens, it will probably cut up. The polar jet stream can mirror this upheaval, turning into weaker or wavy. On the floor, chilly air is pushed southward in some places.
NOAA

Moreover, a hotter ocean results in extra evaporation, and since a hotter ambiance can maintain extra moisture, meaning extra moisture is turning into out there for storms. The method of moisture condensing into rain or snow produces vitality for storms as effectively. Nevertheless, warming can even scale back the energy of storms by decreasing temperature contrasts. The opposing results make it complicated to assess the potential change to average storm strength.

Nevertheless, intense events do not necessarily change in the same way as average events. On steadiness, it seems that the most intense winter storms may be becoming more intense. Moreover, a hotter setting will increase the chance that precipitation that might have fallen as snow in earlier winters could now be extra more likely to fall as sleet and freezing rain.

There are nonetheless many questions

Scientists are continuously enhancing our capacity to foretell and reply to those extreme climate occasions, however there are a lot of questions nonetheless to reply.

A lot of the info and analysis within the subject depends on a basis of labor by federal workers, together with authorities labs just like the National Center for Atmospheric Research, often known as NCAR, which has been focused by the Trump administration for funding cuts. These scientists assist develop the essential fashions, measuring devices and knowledge that scientists and forecasters in all places rely upon.