Thermal Inversion & Pollution (College Board AP® Environmental Science): Study Guide
What is a thermal inversion?
Thermal inversion is a meteorological event
Occurs when a layer of warm air traps cooler air near the ground
Pollutants accumulate in the trapped cool air, leading to high concentrations
This typically occurs during winter nights or early mornings
How thermal inversion occurs
During a thermal inversion, the normal temperature gradient in the atmosphere is changed as the air temperature at the Earth’s surface is cooler than the air at higher altitudes
Thermal inversions occur when cold and warm air masses, high-pressure systems, and topographic characteristics prevent warm air from rising
They can happen anytime, although they are more common in winter when the ground cools faster than the air above it
Inversions are more likely in valleys or areas with minimal wind
Smog and thermal inversion
Thermal inversion traps pollution close to the ground, especially smog and particulates, leading to poor visibility and air quality
During the day the ground heats up, warming the air above
Warm air rises, allowing pollutants to disperse
During the night the ground cools rapidly, cooling the air near the surface
A layer of warm air above traps the cooler air and pollutants

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