Why a Lake Turns Over Twice a Year
In a deep lake in a cool climate, the water is not mixed evenly. For much of the year it separates into layers, and twice a year those layers trade places in an event called turnover. The key to the story is a peculiar property of water: it is densest at about four degrees Celsius, not at its freezing point.
In summer, the sun warms the top of the lake. Warm water is lighter than cold water, so it stays on the surface, floating above a deep layer of cold, dense water. Between them lies a narrow zone where the temperature drops quickly. Wind can stir the upper layer, but it cannot easily push through that barrier, so the bottom water is cut off from fresh air. In a lake rich in nutrients, the oxygen in the deep water may slowly run low.
As autumn arrives, the surface water cools and becomes heavier. Eventually it is as dense as the water beneath it, and nothing holds the layers apart. Wind then mixes the whole lake from top to bottom. This is the fall turnover. It carries oxygen down to the depths and lifts nutrients toward the light.
In winter, the surface may cool below four degrees, becoming lighter again, and ice forms on top. The lake settles into layers once more, this time with the coldest water at the surface. When spring warms the ice and the surface water, the process reverses. The top water sinks until the lake is mixed again, which is the spring turnover. These two mixings keep a lake supplied with oxygen, which is why fish and other animals can live in its depths.