Answer:
In meteorology, an inversion refers to a layer of the atmosphere in which temperature increases with altitude, opposite to the usual decrease with altitude. This occurs when a layer of warm air overlays a layer of cooler air, trapping it below.
Inversions typically form on clear, calm nights when the ground cools rapidly, causing the air near the ground to cool and become denser than the air above it. This can cause the air to become stable, trapping pollutants, moisture, and fog near the ground. Inversions can also form as a result of high-pressure systems, which can bring in warm air aloft that traps cooler air near the surface. Inversions can have significant impacts on air quality, visibility, and weather patterns.
Step-by-step explanation: