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Air Masses. An air mass is a large body of air that has relatively uniform temperature and humidity characteristics. If air remains over a source region long enough, it will acquire the properties of the surface below. They are grouped into four categories based on their source region
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An air mass is a large body of air that has relatively uniform temperature and humidity characteristics. • If air remains over a source region long enough, it will acquire the properties of the surface below
They are grouped into four categories based on their source region • Polar “P”- Cold • Tropical “T”- Warm • Continental “C”- Dry • Maritime “M”- Wet
These letters are combined to indicate the type of air mass:cP: cold, dry air massmP: cold, moist air masscT: warm, dry air massmT: warm, moist air mass
Fronts • When 2 air masses meet • Can be 100s of miles long • Named by which mass Overtakes the other mass
Cold Front • Fast Moving • After there are cold temps • Vertical boundaries • Warm air is pushed up fast • Can lead to thunderstorms • Video from plane • Severe Storm
Warm Front • Distinct Cloud Pattern • Slow Moving • Can lead to days of rainy weather • Gradual Front Line
Occluded Front • Warm air is isolated off of the ground • Heavy Rain • 3 different air masses
Stationary Front • Neither air mass overtakes the other • Extended clouds or rain for days