Ch. 7 Flashcards
source region
regions of earths surface that are particularly well suited to generate air masses. extensive, physically uniform, and associated with air that is stationary or anticyclonic. air masses are classified based on this region
six general classes of air masses in N America
(1) Continental Polar (2) maritime polar (3) maritime tropical (4) Continental Tropical (5) Equatorial (6) Arctic/Antarctic
Continental Polar
cP. central and northern canada. dominant feature in winter with cold, dry, stable nature
Arctic
A. originate further north than the continental polar. colder and drier
Maritime Polar
mP. air from pacific in winter can bring cloudiness and heave rain to mountainous coastal west regions. fog and low stratus clouds in the summer
Maritime Tropical
air from Atlantic/Caribbean/Gulf of mexico is warm moist and unstable. influence weather east of rockies, southern canada and much of mexico serving as the principal precipitin source in this region
Continental Tropical
relatively unimportant in north america. summer hot very dry unstable air surges into the southern great plaines area on occasion bringing heat waves and dry conditions
equatorial
only affect n america in association with hurricanes, provides a ton of rain. high humidity and instability
front
unlike air masses meet and do not readily mix. a narrow three dimensional transition zone
cold front
advancing cold air mass meets and displaced a warm air front. lower portion of air slowed due to friction forming a nose at the front. steep. faster advancing. leads to rapid lifting and cooling of the warm air ahead of the cool air.
warm front
gentle slope. when meets the cool air rises and cools adiabatically usually resulting in clouds and precipitation. clouds form slowly and turbulence is limited.
stationary front
when neither air mass displaces the other. often gently rising warm air produces limited precipitation similar to that along a warm air front
occluded front
when a cold front overtakes a warm front.
midlatitude cyclones
dominate weather maps in the midlatitudes. associated with air mass convergence on regions between about 30 and 70 degrees of latitude. low pressure air, converging counter clockwise circulation.
midlatitude anticyclone
extensive, migratory high pressure cell of the midlatitudes. generally bigger than cyclone and moves west to east with the westerlies. contain no fronts. air converging and moving down and diverging at surface, clockwise in N counter in S. winter: characterized by very low temps.