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#27 | |
Senior Member
Join Date: Apr 2004
Location: Meredith/Naples Florida
Posts: 367
Thanks: 135
Thanked 50 Times in 26 Posts
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![]() Quote:
2. In most Januaries and Februaries, snow both reflects sunlight and insulates the lake. With a thick snow layer, the lake neither gains nor loses heat. The bottom sediment is actually heating the lake water slightly over the winter, from stored summer heat. 3. Around March, as the air warms and the sun gets more intense, the snow melts, allowing light to penetrate the ice. Because the ice acts like the glass in a greenhouse, the water beneath it begins to warm, and the ice begins to melt FROM THE BOTTOM. 4. When the ice thickness erodes to between 4 and 12 inches, it transforms into long vertical crystals called "candles." These conduct light even better, so the ice starts to look black, because it is not reflecting much sunlight. 5. Warming continues because the light energy is being transferred to the water below the ice. Meltwater fills in between the crystals, which begin breaking apart. The surface appears grayish as the ice reflects a bit more light than before. 6. The wind comes up, and breaks the surface apart. The candles will often be blown to one side of the lake, making a tinkling sound as they knock against one another, and piling up on the shore. In hours, a sparkling blue lake, once again! Great description. I can visually see it happening from my perch here in hot humid Florida. And I can remember that tinkling sound and seeing that sparkling blue lake. Can the black flies and mosquitoes be far behind. Time to get the flyrod out. |
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