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Air mass stability affects the type of weather that occurs along or ahead of a

front when one type of air mass overlies another. The air mass itself has very

little changes in temperature and humidity. An air mass is separated from an

adjacent body of air by a transition that may be sharply defined called a front.

The air mass is then determined by the type of front encountered. Prior to

passing of the front the temperature is warm, atmospheric pressure

decreased slightly, winds are south to southeast, there are showers and

cirrus and cirrostratus clouds changing later to cumulus and cumulonimbus

clouds. When the front comes in contact with the air mass there is sudden

cooling of air, the atmospheric pressure levels off then increases, winds are

variable and gusty, there is heavy rain or snow, sometimes even hail and the

clouds are now cumulus and cumulonimbus as mentioned earlier.

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