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Air Masses and Air Mass
Weather
By
Diana L. Duckworth
Rustburg High School
Campbell County Virginia
Air Masses
• Very large body of air with uniform heat
and moisture
– Forms in region with uniform conditions of
heat and moisture
• Source area
• Described by temperatures & humidity
– Use air temperature & dew point temperature
Five Types of Air Masses
• mT Maritime Tropical
– Forms over tropical oceans (low latitudes)
– High humidity & high temperatures
• mP Maritime Polar
– Forms over polar oceans (high latitudes)
– High humidity & low temperatures
• All Maritime air masses have high humidity
Five Types cont’d
• cT Continental Tropical
– Forms over tropical land masses (low latitudes)
– Dry (low humidity) and high temperatures
• cP Continental Polar
– Forms over polar land masses (high latitudes)
– Dry (low humidity) and low temperatures
• cA Continental Arctic
– Forms over the arctic land masses (near poles)
• Very dry & very cold
• All continental air masses are dry
cA
cP
mP
mP
cT
mT
mT
Air Mass Source Regions
• Polar air masses form at high latitudes
• North of Polar Front & Jet Stream
• All polar air masses are cold
• Tropical air masses form at low latitudes
• South of the subtropical Jet Stream
• All tropical air masses are hot
Air Mass Weather
• 75% of the time weather is controlled by
air masses
• Air masses form in one place and move
into another area of different condtions
• Kind of weather depends on two things:
– Difference in temperature between air mass &
ground
– Amount of moisture in air
Tropical Air Masses Move North
• Warm air over colder surface
• Heat flows from air to land (air cools)
• Cold air is stable, does not rise
• Continental air masses dry, clear weather
• Maritime air masses humid, fog forms
when air cools
Polar Air Masses Move South
• Colder air over warmer surface
• Heat flows from land to air, so air gets
warm
• Warm air rises – unstable atmosphere
• Continental air masses – fair weather
cumulus clouds
• Maritime air masses – rising air produces
showers
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