How does lake effect snow stop?

Luckily for people living near large lakes, lake effect snow generally slows down around February. That's when the lakes freeze over, making it impossible for the air to steal moisture away from the lake. Not surprisingly, Buffalo is one of the snowiest cities in the country.



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Due to its relatively shallow depths, Lake Erie has the distinction of being the only Great Lake capable of completely freezing over. As it freezes throughout the winter, and the supply of moisture from the lake surface is cut off, lake-effect snow events cease.

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Lake-effect snow generally doesn't fall over the water because it needs the friction and topography of the land to bring out the snow. Winds usually blow west to east in the Northern Hemisphere, so the lake-enhanced snow is pushed to the eastern side of the Great Lakes, Miller said.

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Syracuse, New York, directly south of the Tug Hill Plateau, receives significant lake-effect snow from Lake Ontario, and averages 115.6 inches (294 cm) of snow per year, which is enough snowfall to be considered one of the snowiest large cities in America.

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Lake-effect snow is a frequent contributor to our seasonal snowfall in Chicago and with Lake Michigan almost ice free, the lake-effect snow machine is open for business provided a cold wind is blowing in our favor in the right direction. Nearly 93% of the Great Lakes does not have significant ice cover.

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Anywhere! Lake effect snow can occur over any unfrozen body of water where the fetch is long enough to gather enough moisture to create snow. Lake effect snow can occur over Lake Tahoe, the Great Salt Lake, the finger lakes, and even has been reported over rivers in the Midwest!

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