On a clear, calm anticyclonic night, the cool air may roll downhill and accumulate in valleys, and the air temperature will be lower near the valley bottom than it is 100m to 200m (328–656ft) higher. Above the cold layer there will be warmer air, which is likely to form cloud or haze. Evidence f a temperature inversion can be seen if there is smoke rising from a bonfire. The smoke will rise vertically and then bend horizontally when it reaches the inversion layer. If this situation develops on a larger scale, dust and other particulates rising into the atmosphere are trapped and unable to escape, giving rise to serious pollution.
Related category ATMOSPHERIC PHENOMENA AND STRUCTURES
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