Part 3. Distribution and Movement of Air Chapter 9 Air Masses and Fronts.
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Transcript of Part 3. Distribution and Movement of Air Chapter 9 Air Masses and Fronts.
Part 3. Distribution and Movement of Air
Chapter 9
Air Masses and Fronts
IntroductionAir masses are large volumes of air that contain uniform temperature and humidity characteristics
Different air masses have different source regions
Air mass properties can modify as the air mass travel over continents and oceans
Air mass properties will modify as the air mass moves north or south
Fronts are the boundaries between air masses
North American air masses and source regions
Continental Polar (cP) and Continental Arctic (cA) Air Masses • Canada and Asia origin for North America• Cold and dry• Inherently stable
Continental Polar AirArctic Air
cP Air Migration and Modification
Maritime Polar (mP) Air Masses• Upper latitude ocean origin
• Cool and moist
Continental Tropical (cT) Air Masses• Desert southwest of U.S. and northern Mexico origin
• Hot and very dry
• Inherently unstable
Maritime Tropical (mT) Air Masses• Low latitude ocean origin (Gulf of Mexico)• Warm and moist• Inherently unstable
Weather map symbols that show the four types of fronts between air masses
• Cold fronts– Cold air displaces warm air– Steep uplift of the warm air causes
cumulonimbus clouds and precipitation
Frontal development
Vertical lifting of warm along a cold front
A cold front depicted on a satellite picture (a) andradar composite (b)
• Warm fronts– Warm air overruns and displaces colder
air– Lifting along a warm front usually
produces stratus clouds and often light precipitation
• Stationary fronts– Neither air mass on either side of the
front can make the front move very much– The warmer air can move aloft over the
colder air at a stationary front
Profile of a warm front
• Occluded fronts form when a cold front overtakes a warm front. The front at the surface divides two cold air masses, while the warm air is aloft over the front.
– Cold-type occlusion has a colder air mass pushing out a cooler air mass
– Common in the eastern half of North America
– Warm-type occlusion has a cooler air mass pushing out a colder air mass
– Common along the western edge of North America
Occlusion sequence (next three slides)
Some occlusions form when the surface low elongates and moves away from the junction of the cold and warm fronts
Some occlusions form when the intersectionof the cold and warm fronts slides alongthe warm front
• Drylines are fronts with little temperature change but a strong humidity contrast
– Often form when cT air moves into mT air
Continental Tropical Air
Maritime Tropical Air