When is lake turnover




















For many lakes deeper than about 20 feet, distinct, thermally stratified layers of water form during the summer. These layers prevent the lake from mixing and aerating. Warmer and less dense water floats on the top of cooler, denser water at the bottom. Temperature layering begins to weaken when outside temperatures cool.

This allows the lake to mix when temperatures equalize throughout the water column. Meaning, water from the bottom of the lake rises to the top, and water from the top of the lake sinks to the bottom. The process allows for oxygen to be replenished and nutrients to be distributed throughout the lake. On the other hand, shallow lakes like Lake Wingra maintain a more uniform temperature.

Shallow lakes mix frequently and rarely experience stratification. Water is unique in the way it changes density at different temperatures. Unlike almost all other liquids, water is most dense at 39 degrees Fahrenheit 4 degrees Celsius , and is lighter at both warmer and colder temperatures. In other words, when water reaches the critical temperature of 39 degrees Fahrenheit, further cooling causes the water molecules to become less dense and rise to the surface.

This unusual characteristic allows water to form distinct layers within an otherwise uniform liquid. This phenomenon explains why ice forms at the surface and does not sink. There are two ways that help visualize this phenomenon. Land Management. Small Game. How To. Wild Game Recipes. Country Roots. View All. The Mossy Oak Store.

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