Normally, the temperature of air is cooler up high and warmer down below. This occurs because warm air expands and cools as it rises. A temperature inversion is when the temperature of air is warmer up high and cooler down below.
There are two types of temperature inversions:
Surface Inversions: temperature inversions which occur near the Earth's surface
Aloft Inversions: temperature inversions which occur above the ground
Conditions that favor the formation of a temperature inversion include: long nights (winter), clear skies, and calm winds. Geologic features such as valleys may enhance the formation of temperature inversions. A temperature inversion may last for several days.
Temperature inversions can create several problems:
- Temperature inversions can trap pollutants near the surface and contribute to poor air quality.
- Temperature inversions can trap sound near the surface and may cause noise to sound louder.
- Temperature inversions may prevent thunderstorms from forming.
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