Chapter Eight - Test Three Flashcards
What is an Air Mass?
An immense “body” of air (thousands of km2 across, and several km thick) dominated by High Pressure whose: Thermal and moisture properties remain homogenous in any direction within the air mass.
When the air mass moves out of its region of origin, it will carry these T and Td characteristics with it
Thermals property: Temperature (T)
Moisture property: Dewpoint (Td)
Source Regions
Air masses develop over regions of uniform geography, usually flat
regions of similar composition (i.e. sand, water, ice) that are:
Conducive to the formation of high pressure
Examples: Gulf of Mexico
Deserts of Mexico
Tundra of northern Canada
Atlantic and Pacific Ocean
The longer an Air Mass remains stationary over its Source Region, the more likely it will…
acquire the thermal and moisture properties of the surface
Classifying Air Masses
Depends on the latitude and nature of the underlying surface.
Classifying Air Masses
For latitude, we designate:
arctic, polar or tropical, which determines thermal properties
Classifying Air Masses
For surface, we designate:
continental or maritime, which determines moisture properties
Air Mass cA cP cT mT mP What about Basic Thermal or Moisture properties?
Basic Thermal, Moisture Properties cA Very cold Dry (winter only) cP Cold Dry cT Hot Dry (summer only) mT Warm Moist mP Cool Moist
Remember that all four air mass types are characterized by ____
high pressure
The typical movement of the four major air
masses is controlled by the:
Jet Stream
Continental Polar (cP) and Continental Arctic (cA) Air Masses
Characterized by very cold (cA) or cold (cP) and dry air
North American Air Masses are characterized by very cold (cA) or cold (cP) and dry air
Cold : because of the long nights in the high latitudes (i.e. little solar radiation)
lack of water vapor in the air results in maximum, almost continuous radiational cooling
Dry : because the air originates over land and/or frozen ArcticOcean and because cold air holds very little water vapor
cA (form over Arctic Basin) and cP (form over northern Canada) air masses originate over flat snow/ice covered areas and generally move south-southeast into the US, responsible:
- coldest air in the winter: “Siberian Express” (Box 8.1)
- Lake Effect snow storms (Box 8.2)
Maritime Polar (mP) Air Masses
Originate over the northern Pacific and Atlantic Oceans
North American Air Masses are characterized by cool and moist air (mP)
Cool : because it originates over the northern oceans, which are always cool (but never frozen)
Moist: because the air originates over open oceans where water vapor is plentiful