Weather word of the week: temperature inversion.
A temperature inversion is a layer in the atmosphere in which air temperature increases with height. This is most commonly seen at night, when there are clear skies with little to no wind. The air near the ground cools quicker than the air aloft.
A temperature inversion is a layer in the atmosphere in which air temperature increases with height. This is most commonly seen at night, when there are clear skies with little to no wind. The air near the ground cools quicker than the air aloft.
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