![]() | This is Pink Lake in Gatineau Park. It was named after somebody named Pink. An unusual lack of circulation ibetween the layers of water in this lake has resulted in oxygen depletion which is the root cause of its striking green colour. |
Larger lakes can also modify the climate in nearby areas. They provide a source of moisture for rain or snow. Also, water absorbs heat and then re-releases it relatively slowly.
As water cools, it becomes more dense until 4 degrees Celsius, at which point, it becomes less dense as it cools until it freezes at 0 (zero) degrees Celsius. Because water tends to form layers of equal density, this means that, as the temperature cools in the fall, most northern lakes tend to "turn over" before they freeze over (if they do). As the lakes warm up in the spring, a second "turn over" usually happens. In the summer, the coolest water will be found at the bottom. In the water, it is usually the warmest water at the bottom. In some deep lakes, the lower levels may not "turn over".