What is the paradox of lake effect snow?

The climate around Lake Superior is colder than that around other Great Lakes, which makes it more able to support snowfall for a longer period of time, even when temperatures warm. Eventually, though, as temperatures continue to rise, lake effect snows turn into rain.



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Lake Effect Snow (LES) is very common across the Great Lakes region during the late fall and winter. LES occurs when cold air, often originating from Canada, moves across the open waters of the Great Lakes.

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Lake Ontario and Lake Erie Snowbelts The region east and southeast of Lake Ontario frequently sees daily snowfall totals that are higher than anywhere in the United States. Syracuse, New York, receives significant lake-effect snow from Lake Ontario, averaging 116 inches (294 cm) of snow per year.

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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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Lake-effect snow can form on small lakes just as it does in the Great Lakes. Salt Lake City, Fort Worth and Carson City, Nevada have all had bouts of snow from lakes. Inland lake-effect and ocean-effect doesn't just occur in the United States.

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Lake effect snows are common downwind of the Great Lakes in the United States and Canada, the Great Salt Lake in Utah, and in parts of Scandinavia, Korea, and Japan.

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