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Weekend winter storm that battered eastern U.S. was supercharged by climate change

A warmer atmosphere can hold more moisture, and that’s why last weekend’s winter storm dumped more snow, sleet and freezing rain than similar weather systems might have in the past

A snow-covered road with cars buried on either side going off into the distance. A person in the middle distance is shoveling out their car.

People dig out their cars parked along Lancaster Street during a winter storm on January 26, 2026, in Albany, N.Y.

Lori Van Buren/Albany Times Union via Getty Images

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If you live in the eastern U.S., you are likely among the millions dealing with the aftereffects of the heavy snow, sleet and freezing rain that buried the region over the weekend. And while it may be extremely cold, new research reveals that last weekend’s weather was in fact supercharged by global warming.

Some of the hardest hit places saw more than two feet of snowfall, while up to an inch of ice from freezing rain shut down roads and cut power throughout the Southeast. No doubt, this storm was big. It was always going to pack a punch—but it dumped more frozen precipitation than it would have if the storm had occurred decades earlier. It may seem paradoxical that a warming climate could mean heavier snowfalls, but hotter, albeit still below freezing, temperatures are nonetheless a recipe for more snow.

That’s because for every one degree Celsius (1.8 degrees Fahrenheit) of warming, the atmosphere can hold about 7 percent more moisture. And this storm happened in an atmosphere that has become up to five degrees C (nine degrees F) warmer than it was in past decades, according to the research organization ClimaMeter, which produced the new analysis. That means that this storm had up to 20 percent more precipitation than it would have if there was no human-caused warming.


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Some regions of the U.S. could see more snow for a time as the planet’s temperature rises—particularly those places prone to lake-effect snow, because bodies of water take longer to freeze over in winter.

The effect of climate change on snowstorms means that “infrastructure and emergency planning standards, historically based on past snowfall records, may no longer be sufficient,” said analysis co-author Haosu Tang of the University of Sheffield in England in a statement.

Andrea Thompson is senior editor for Earth and environment at Scientific American, covering the environment, energy and Earth sciences. She has been covering these topics for nearly two decades. Prior to joining Scientific American, she was a senior writer covering climate science at Climate Central and a reporter and editor at Live Science, where she primarily covered earth science and the environment. She has moderated panels, including as part of the United Nations Sustainable Development Media Zone, and appeared in radio and television interviews on major networks. She holds a graduate degree in science, health and environmental reporting from New York University, as well as a B.S. and an M.S. in atmospheric chemistry from the Georgia Institute of Technology. Follow Thompson on Bluesky @andreatweather.bsky.social

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