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Lake Effect

Gemini Sparkle

Key Takeaways:

  • Lake effect weather, common downwind of large bodies of water like the Great Lakes from November to March, is characterized by heavy, localized snow and ice-laden clouds.
  • This phenomenon occurs as air picks up moisture over the water and dumps it on land, typically affecting areas within 10-100 miles downwind.
  • Pure lake effect clouds generally top out below 10,000 feet, but can combine with other weather systems, potentially intensifying effects and creating conditions with no ice-free altitude for aircraft.
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The downwind sides of any large body of water—and especially the Great Lakes—can be perennial winners of the rotten-weather-in-winter prize. The air moving across them picks up moisture, then dumps it in the form of snow from heavy, ice-laden clouds over the downwind land area. The cloud cover almost invariably harbors ice and generates localized heavy snow fall, especially in the roughly 10-mile strip of land nearest the lake.

No matter what the forecast, there’s a safe rule of thumb for airports within 50 miles east or south of one of the Great Lakes: From November through March, it’s wise to be ready for lake effect clouds, ice and snow if the surface wind is stronger than a light breeze. It’s not unusual for such conditions to extend 100 miles or more downwind. Tops are usually at or below 10,000 feet and—generally, unless there’s an associated weather system—clear above.

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