Since water is good at holding heat, the more water there is, the more heat it will hold. This is why large deep lakes take longer freeze and melt than small shallow lakes.
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Think of it this way: Shallower water allows more rapid mixed cooling to the freezing point of upper lake layers. This is why on any lake you'll usually see the near-shore shallow water freezing before more distant deeper water.
Most lakes and ponds don't completely freeze because the ice (and eventually snow) on the surface acts to insulate the water below. Our winters aren't long or cold enough to completely freeze most local water bodies. This process of lakes turning over is crtically important to the life in the lake.
As the density of the water rises, so does its temperature. At its deepest point the water in Lake Lunz remains constant at four Celsius. A lake more than one meter deep will never freeze completely, meaning there's plenty of space for animal and plant life to survive the winter.
Since water is good at holding heat, the more water there is, the more heat it will hold. This is why large deep lakes take longer freeze and melt than small shallow lakes. Water freezes from the perimeter of the lake to the center.
Your lake or pond won't fully freeze when the water temperature drops below 32 degrees. You should also consider what outside factors may be affecting your body of water. How much sunshine does the area get?
If you can see the ground through the ice, then there's going to be warmer water under it. Out in the middle, the ice grows thicker over the cold dark depths. Also, ice always melts away from the shore first.
But, in winter some lake surfaces can get very cold. When this happens, the surface water becomes more dense than the deeper water with a more constant year-round temperature (which is now warmer than the surface), and the lake turns, when the colder surface water sinks to the lake bottom.
Colder than 4° Celsius (39° Fahrenheit), water begins expanding and becomes less dense as it gets colder. As a result, close to freezing, colder water floats to the top and the warmer water sinks to the bottom. The density of water as a function of temperature can be seen in the plot on the right.
The reason water freezes from the top down is because, unlike almost everything else, water gets less dense when it freezes. This is why ice cubes float in a drink.
Health risksWinter swimming can be dangerous to people who are not used to swimming in very cold water. After immersion in cold water the cold shock response will occur, causing an uncontrollable gasp for air. This is followed by hyperventilation, a longer period of more rapid breathing.