As surface water cools to 4°C, it sinks, displacing warmer water until the entire lake is near 4°C. Further surface cooling creates less dense, near-freezing water that stays on top and forms ice. This insulates the dense, liquid 4°C water layer at the bottom, allowing aquatic life to survive.
As surface water cools to 4°C, it sinks, displacing warmer water until the entire lake is near 4°C. Further surface cooling creates less dense, near-freezing water that stays on top and forms ice. This insulates the dense, liquid 4°C water layer at the bottom, allowing aquatic life to survive.