chapter 8 air masses. air mass - large mass of air characterized by: (1) common properties of...
TRANSCRIPT
CHAPTER 8
Air Masses
Air mass
- Large mass of air characterized by:(1) common properties of temperature and humidity(2) characteristics of their region of
origin source region
- Air mass is important concept in meteorology
Source Region
- Term for a region whose conditions create air masses
- Ideally it should meet the criteria of:(1)Extensive and uniform in area(2) Area of air stagnation
Air mass source regions are found in high and low latitude regions
Source Region, cont
- They will migrate to the mid-latitudes- They make the mid-latitudes a
conflict zone- Aside: This idea of a conflict zone
became an important aspect of the writings of Ellsworth Huntington and the
paradigm of environmental determinism
Source Region, cont
- Air masses are classified by:(1) latitude of the source region
Latitude SymbolArctic APolar PTropical TEquatorial EAntarctica AA
* differences are relative
Source Region, cont
- Air masses are classified by:(2) surface-type of the source region
Surface Type Symbol continental c marine m
Air Mass
- Taken Together:Air Mass Symbolcontinental arctic cAcontinental polar cPcontinental tropical cTmarine tropical mTmarine polar mPmarine Equatorial mEcontinental Antarctic cAA
Air Mass, cont
- In addition, we frequently add a 3rd factor (3) tendency --- if air mass is colder than the surface it
passes over, a “k” is added after its initial symbols (cAk – continental arctic air colder than surface passing over)--- if air mass is warmer than surface passed over, a “w” is added (mTw – marine tropical air warmer than surface passed over)
Air Mass, cont
- “k” and “w” are indicators of stability tendency
--- “k” situation leads to instability
--- “w” situation leads to stability
- The air mass both modifies and is modified by the surface it passes over after leaving source region
Air Mass, cont
- Air mass influence on North America--- cP and cA--- mP--- mT--- cT
Air Mass, cont
- cA and cP--- dry and cold--- originate over central Canada (cP) and Greenland and the highArctic (cA)
*Distinguished by relative difference in temperaturecP-very cold cA-bitter
Air Mass, cont
cA and cP - Greatest effect during N.A. winter (land&air
very cold)… may bring brief cool/clear summer weather
- Invades the central U.S. ; no mountains- When crossing open Great Lakes will bring
precipitation and in winter produces lake-effect snows
Air Mass, cont
mT- Originate Caribbean and Gulf of Mexico,
lesser so tropical Pacific… Pacific air has little effect N.A., though it
can bring extensive July-Aug precipitation of SW
- Warm to hot. Humid and unstable- Dominant summer air mass of central U.S.- Potential for extensive precipitation and
violent weather patterns
Air Mass, cont
mP- Forms over high latitude oceans
… may have originated as cP air over Siberia (modified over Pacific)
- Cool to cold; humid and unstable compared to cP and cA
- Because of westerly air flow, Pacific mP more important to N.A. than Atlantic
- Potential for heavy orographic effect
Air Mass, cont
cT- N.A. doesn’t have the land mass form
extensive cT air- However, Mexico and the desert SW U.S,
produce the hot, dry air- Air is unstable, but unlike other tropical
air masses, cT is dry unstable- Generally confined to source region,
may break out during very hot, dry seasons – brings drought the Great Plains