Final Exam Flashcards
Primary Circulation
general global circulation: average air flow around globe and created by unequal heating of earth’s surface
Secondary Circulation
related to pressure belts migratory high pressure and low pressure systems
Tertiary Circulation
includes local winds and temporal weather patterns
General Atmospheric circulation
reason there is different weather patterns, jet streams, deserts, and prevailing winds; caused by rotation of Earth and amount of heat different parts of Earth receive.
Air mass
a large body of air with similar temperature and moisture characteristics in any horizontal direction
Air mass and Earth’s surface
each area of Earth’s surface impacts its temperature and moisture characteristics to overlaying air; Effect of the surface on the air creates regional air masses w/ homogenous mix of temperature, humidity, and stability
Classification of air masses
air masses are classified moisture and temperature
Moisture
“m” for maritime (wet) & “c” for continental (dry)
Temperature
“A” for arctic, “P” for polar, “T” for tropical, “E” for equatorial, & “AA” for antartic
Four categories for the classification of air masses
(cP, mP, cT, mT)
cP
continental polar: air masses form only in Northern Hemisphere and developed in cold weather conditions; displaces moist and warm air: producing lifting, cooling and condensation
mP
maritime polar: air masses in the Northern Hemisphere exist over the northern oceans
mT
maritime tropical: two maritime tropical air masses that influence North America
mT Gulf/ Atlantic:
unstable and active in spring and fall
mT pacific:
stable to conditionally unstable and generally lower in moisture content and available energy
cT
continental tropical: hot dry unstable at low levels, stable at upper levels, over Mexican plateau region
If air mass is colder than surface over which it is moving
“k” is added
If air mass is warmer than the surface over which it is moving
“w” is added
Zonal flows (winds)
move east or west along parallels of latitude
Meridional flows (winds)
move north or south along meridians or parallels to lines of longitude
Intertropical Convergence Zone (ITCZ)
Where northeast trade winds in the northern hemisphere and the southeast trade winds in the southern hemisphere meet
NE and SE Trade winds
comes from the east located between the equator and 30 degrees latitude in both hemispheres
Doldrums
another name for intertropical convergence zone
Horse latitudes
around 30 degrees latitude, sinking air creates a belt of high pressure which causes weak winds
Pacific High
moves northward during summer, during winter moves south allowing precipitation to SW US