Subsidence in the
Earth's atmosphere is most commonly caused by low temperatures: as air cools, it becomes denser and moves towards the ground, just as warm air becomes less dense and moves upwards. Cool subsiding air is subject to
adiabatic warming which tends to cause the evaporation of any clouds that might be present. Subsidence generally causes high
barometric pressure as more air moves into the same space: the
polar highs are areas of almost constant subsidence, as are the
horse latitudes, and these areas of subsidence are the sources of much of the world's
prevailing wind. Subsidence also causes many smaller-scale
weather phenomena, such as morning fog. An extreme form of subsidence is a
downburst, which can result in damage similar to that produced by a tornado. A milder form of subsidence is referred to as
downdraft.