Why Fog Pools in Valleys at Dawn
On a calm, clear morning, people who live in hills often see a strange sight. The valley floor is filled with a thick white fog, like milk in a bowl, while the hilltops above it shine in the sun. The fog is no accident. It follows from how air behaves after dark.
When the sky is clear at night, the ground loses its heat and cools off. The air touching the ground cools too. Cold air is heavier than warm air, so on a slope it slowly slides downhill, much like water would, and collects in the lowest places. Valleys end up as pools of the coldest air.
Air always holds some water vapor, but cold air can hold less of it. When the air in the valley gets cold enough, the vapor can no longer stay invisible. It turns into countless tiny drops floating close to the ground. That cloud at ground level is fog.
Fog like this lasts only until the morning sun warms the ground. As the air heats up, the drops change back into vapor, and the fog thins and vanishes. Drivers are told to slow down in fog, because they cannot see far ahead.