Aviation Weather: Air Masses & Fronts

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Last updated 10:08 PM on 10/9/26
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27 Terms

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Air Mass is

High/low pressure

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What is air masses and fronts?

A large body of air with general uniform tempature and humidty.

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What do air Masses and front range from?

Poles to desert to tropical climates

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How are Air masses classified?

By tempature and moisture properties of their source regions.

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What does air masses moisture contain of:

Continental ( c ) and Maritime (m)

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What does air masses tempature contain of?

Artic (a), Polar (P) and Tropical (T)

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What is the High continental pressure?

Continental Polar (cP) - cold, dry

Continental Artic (cA) - cold, dry


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How is high pressure characterized?

Cooler, dense air masses causing sinking air (if it cold, its high pressure)

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What is the Low continental pressure?

continental Tropical (cT) - warm, dry
Maritime Polar (mP) - cool, moist
Maritime Tropical (mT) - warm, moist

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What are fronts?

a boundary or transition zone between different fronts

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What are the 5 different front?

Cold front, warm front, stationary front, occluded front, and dry line.

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What is warm fronts?

Occurs when a mass of air mass advances and replaces a body of cold air.

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What is cold fronts?

Occurs when a mass of cold, dense and stable air advances and replaces a body warmer air.

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How fast does warm fronts move

Slow at 10-25 miles per hour

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How fast does cold fronts move?

Move fast at 25-30 miles per hour

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What is stationary front?

A front that stalls or is moving very slowly over an area.

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What is occluded front?

When a cold front will “catch up” to the warm front and will collide with it forms ______

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What is cold front occulsion?

Happens when the cloud front overtakes the warm front and the air ahead of the warm front.

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What is warm front occulsion?

Occurs when the air behind the cold front is actually not as cold as the cool air mass ahead of warm.

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What is a wave cyclone model?

Is low pressure circulation that forms and moves along a front.

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First stage is

Stationary: all wave cyclones startes as stationary fronts

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Stage two is

Frontal wave: Disturbance or upper level jet streams shifts create a wavelike or bend along the stationary front.

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Stage three is

Open wave: Distinct cold & warm fronts become fully organized and seperated by warm sectors

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Stage four:

Occluding Stage: The faster moving cloud front catches up to and overtakes the slower warm front.

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Stage five:

Dissipation Stage: The surface low - pressure system cut off from its warm air energy source and loses upper level jet stream support.

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What is Dry Line?

This is low - level boundary hundreds of miles long seperating a moist air mass and dry air mass.

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What is a dry line weather?

Since drier air is more dense than moist air, the dry line forces moist air up into Atmosphere as it moves east.