Inversion occurs in
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A ground inversiondevelops when air is cooled by contact with a colder surface until it becomes cooler than the overlying atmosphere; this occursmost often on clear nights, when the ground cools off rapidly by radiation. If the temperature of surface air drops below its dew point, fog may result.
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Inversion Layers. In a typical situation, the atmosphere (with regard to the troposphere) becomes cooler as elevation increases. An “inversion” occurs when a section of the atmosphere becomes warmer as the elevation increases.
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