define the temperature Inversion
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Define the temperature Inversion
In meteorology, an inversion, also known as a temperature inversion, is a deviation from the normal change of an atmospheric property with altitude. It almost always refers to an inversion of the thermal lapse rate. Normally, air temperature decreases with an increase in altitude.
What are the causes of temperature inversion?
Temperature inversions are a result of other weather conditions in an area. They occur most often when a warm, less dense air mass moves over a dense, cold air mass. This can happen, for example, when the air near the ground rapidly loses its heat on a clear night.
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