Cool Air Acts As A Barrier Over Which Warmer Less Dense Air Rises In A Process Known As

The process where cool air acts as a barrier over which warmer less dense air rises is called when the environmental lapse rate is greater than the dry adiabatic rate air is. Imagine that you are on the ground in the wintertime under a cold winter air mass with a warm front approaching. Along a warm front a warm air mass slides over a cold air mass.

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