inversion of temprerature
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It is a reversal of the normal behavior of temperature in the troposphere. Under this meteorological phenomenon a layer of warm air lies over the cold air layer.
It is caused in stac atmospheric conditions while some times, it occurs due to horizontal or vertical movement of air.
Temperature inversion is usually of short duration but quite common nonetheless.
It is caused in stac atmospheric conditions while some times, it occurs due to horizontal or vertical movement of air.
Temperature inversion is usually of short duration but quite common nonetheless.
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