- clear skies
- light winds
- shallow layer of cool moist air near the ground
- long nights
Valley fog forms on clear winter days when heavy cold air settles into the mountain valleys while warmer air moves over the surrounding mountains. Fog forms when the frigid ground cools the air immediately above it. The cooling air thickens into fog as water condenses. Air farther from the Earth’s surface is warmed by the sun, trapping the layer of cold air beneath it. The condition is called a temperature inversion, and it can last several days.When the fog begins to clear it typically moves from north to south down the lake. From the deck of our float cabin we can often see it flowing back through First Narrows.
Thanks for visiting! -- Margy
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