| MadSci Network: Physics |
Kinetic energy is certainly a factor in how rivers freeze. Ambient air temperature is another. Rivers begin freezing at the banks, in pools or eddies. As the ice sheets there grow out into the water, they break off and float downstream. Along with the colder weather both at your location and at the head of the river, this has the effect of cooling the water, regardless of its speed, to near freezing. This accelerates the growth and thickening of ice near the bank, allowing it to reach farther into the moving water, and it also allows any unmelted floes to grow. Most rivers have shallow regions or islands, and floes can become grounded on these. As the floes ground, they provide not only seeds for more stationary ice to form, but blockages which catch other loose ice. Eventually the river surface freezes completely. Even though a river may be covered with ice, you cannot assume the ice is very thick. Even in shallow rivers in cold winter climates, there may be regions where the ice never reaches a thickness of more than a few centimetres. More than one skidooer has gone to his death thinking a frozen river was a great place to open the throttle.
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