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Weather and Climate Ch9
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air masses
a large body of air having more or less uniform temperature and moisture.
fronts
Air masses are commonly separated from each other by fairly narrow boundary regions called fronts
source regions
The areas of the globe where air masses form
Continental polar (Cp) air masses
Air masses thhat form over large, high latitude land masses
Continental Arctic (cA) air masses
colder than continental polar air and is separated from cP by a transition zone called the arctice front
Maritime polar (mP) air masses
similar to continental polar air masses but are more moderate in both temperature and dryness
northeasters
winds that can bring snowfall and cold winds in response to Maritime polar air masses
Continental Tropical (cT) air masses
forms in summer over hot, low latitude areas
Maritime Tropical (mT) air masses
develop over warm, tropical waters and are warm, moist, and unstable near the surface. Can form precipitation and clouds.
cold front
occurs when a wedge of cold air advances toward warm air
warm front
occurs when a wedge of warm air advances toward cold air
stationary front
similar to a cold front but does not move
occluded front
appear at the surface of the boundary of two fronts, but unlike the other three types of fronts, do not separate air masses
overrunning
warm air sliding over a dense cold air mass because the deifferent densities in the two air masses discourage mixing
drylines
areas where mT air and cT air masses reside next to each other
Author
Anonymous
ID
97858
Card Set
Weather and Climate Ch9
Description
Weather and Climate Ch9
Updated
2011-08-22T02:59:11Z
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