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20 Cards in this Set

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Air Masses

large volumes of air that have distinctive characteristics oftemperature and moisture.

cP, cT, mP, mT

Continental Polar, Continental Tropical, Maritime Polar, Maritime Tropical


Continental: Dry


Maritime: Wet


Polar: Cold


Tropical: Warm

Cold Front

The colder air is pushing intothe area occupied by the warmer air mass. This is characterized by cumulus clouds, shorter rain duration, intense weather.

Warm Front

The warmer air pushing into the areas occupied by colder air. This is characterized by stratus clouds, longer period of rain, more chill.

Occluded Front

A cold front will overtake a warm front and the result is that the whole warm frontis lifted off the ground.

Dryline

When two fronts have the same temp but different moisture, they don't mix. In lubbock, it tends to be dryer on the west side of the dryline and wetter on the east.

Cyclones & Anticyclones

Zones of low pressure are called cyclones and zones of highpressure are anticyclones

Polar Front

Where warm tropical air and cold polar air converge.

Rossby Waves

The undulations of the Polar Fronts

Polar Jet Stream

The insanely strong winds along the Polar Fronts.

Cyclogenesis

The formation of a cyclone.

The formation of a cyclone.



Thunderstorms

Rapidly rising air forming cumulonimbus clouds that thunder and lightning and rain heavily.

Köppen System

Identifying climate regions based on temperatureand precipitation over the year.

A Climates

Found roughly between about 20° northand south. Very hot, little variation between seasons, equator, yo.

B Climates

Arid and semiarid regions are, obviously, areas of little water. Deserts and the like.

C Climates

Mesothermal climates: moderate temperatures, hence thename, and occur in the mid-latitudes.


More than half of human population lives in C climates

D Climates

Microthermal climates are characterized by long and cold wintersand short summers. Poleward of C climates.

E Climates

The Polar climates: Ice Cap and Tundra Climates

H Climates

Highland Climates found at any place on earth if there is high enough mountains.

Continentality

A measure of the difference between continental and marine climates characterized by the increased range of temperatures that occurs over land compared with water.