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Lake Effect

Gemini Sparkle

Key Takeaways:

  • Lake effect snow occurs when air gathers moisture over large bodies of water (like the Great Lakes) and deposits heavy, localized snow on downwind land areas, typically from November through March with strong surface winds.
  • These conditions involve ice-laden clouds, generate significant snowfall (especially within 10 miles of the shore), and generally have cloud tops at or below 10,000 feet, often extending 100 miles or more downwind.
  • Lake effect can combine with and intensify other weather systems; if cloud tops exceed 18,000 feet, another system is involved. Pilots should anticipate ice and snow, potentially staying grounded if an ice-free altitude is not safely reachable.
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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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