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On Flat Lake Time
- a Modern Survivor's Guide to Living off the Road System in Alaska

The Freezing of Lakes
Water – 36oF six inches down

In the beginning of September it was a bit chilly crossing the lake in the mornings before sunrise, so we started wearing our winter coats. One of my friends at work asked if the lake was freezing yet. He was surprised that it wasn’t doing so, not even a skim of ice.  I thought  it

                                                                                             strange that he didn’t know how lakes freeze because he is a chemist. I guess it was more the biologist than the chemist in me that made me understand freezing water. It is important to a chemist that pure elements and compounds have specific freezing points, but to a biologist it could be a matter of life and death for an organism and the unique properties of water may well have been a significant condition for the creation of life.
           
One of these unique properties so well evidenced on Flat Lake was that water has a maximum density at 4 degrees centigrade (39.2 degrees Fahrenheit). As the water on the surface of the lake cools and its molecules reach 4 degrees C, the dense water sinks to the bottom of the lake, causing any warmer water to take its place on the surface. As the layer of dense water on the lake bottom deepens, the interface, or thermocline, between it and the warmer layer of water above, rises. When the thermocline reaches the surface, the lake has turned over and can cool further, then freeze.
            Thus, gradually, the whole lake reaches 4 degrees C before the surface can get any cooler. It is only after the entire water column has turned over and the thermocline has reached the surface in this manner that the surface water can cool below 4 degrees C to 0 degrees C and freeze. I use the term water column here because the shallower areas of the lake freeze first since the water column there has less water to turn over. It is usually not the case that an entire lake turns over and freezes at once, but if it has been windy, keeping the surface from freezing, the water temperature can fall below 32oF, or supercool. Then everything can freeze at once when the wind calms, a process Carolyn refers to as slamming shut.
                               

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