Geography 101 The Physical Environment
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Weather Systems:
Air Masses and Fronts

Air Masses

  • Vast pool of air with (fundamentally) the same temperature and moisture characteristics over its horizontal extent.

Air Mass Source Regions

Characteristics

  • Flat terrain

  • Little wind

  • High Pressure

Air Mass Classification (based on:)

Moisture

  • m for maritime

  • c for continental

Temperature

  • A for Arctic (60o - 90o N)

  • P for polar (40o - 60o N or S)

  • T for tropical (15o - 35o N or S)

  • E for equatorial (15o N - 15o S)

  • AA for Antarctic (60o - 90o S)

Air Mass Types

    N. American air masses


Generalized Map of Global Air Masses

Air Mass modification

Examples

  • cP air warms when moving south (cPk); enhances instability

  • mT air cools at surface when moving over a cold ocean current (mTw); enhances stability

Fronts

  • boundary between contrasting masses of air.

Semi-stationary fronts

  • Polar Front - boundary between tropical and polar - type air.

  • Arctic Front - boundary between polar and arctic - type air.

"Weather" fronts

Cold front     

  • Cold air replaces warm air at a location.

  • Steep frontal surface.

  • Vertically developed, cumulus-type clouds.

  • Heavy precipitation of short duration.


Click image to enlarge

Warm Front

  • Warm air replaces cold air at a location.

  • Gentle frontal surface.

  • Layered, stratus-type clouds.

  • Light precipitation of long duration along front.


Click image to enlarge

Occluded Front

 


Click image to enlarge

Stationary Front

  • Little to no horizontal movement. Stays in place.

 

 

Continue to Midlatitude Weather

 


 

 

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© Michael Ritter mritter@uwsp.edu
Last revised March 11, 2007