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Air Masses and Weather Video
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Origin of an Air Mass Air Mass: A large body of air in the lower troposphere that has similar characteristics throughout Characteristics: Several kilometers in diameter Several kilometers high Temperature and humidity are nearly uniform throughout an air mass
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What type of characteristics does as air mass have throughout?
Similar
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Temperature and Moisture Level
These characteristics depend on where the air mass originates. Ex: if an air mass stays in a polar region for an extended period of time, it becomes cold as well. When an air mass travels from one area to another, it takes with it the temperature and humidity of its place of origin As it travels, its characteristics may change
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What happens when an air mass travels?
it takes with it the temperature and humidity of its place of origin
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Types of Air Masses Classification of air masses is based on their place of origin The names are two part: Temperature- arctic, polar, or tropical region Humidity- land (continental) or marine (maritime)
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What two characteristics are used to classify air masses?
Temperature and humidity
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Continental Arctic Originate in Arctic regions
Air becomes extremely cold Capable of causing extreme cold waves as they move into new regions Very dry
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Continental Polar Originate over the inland regions of Alaska and Canada Slightly warmer than Continental Arctic Usually dry If travels over large body of water, can create precipitation
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Maritime Polar Originate over the ocean in high latitudes
Cold and damp Produces fog, clouds, and precipitation “nor’easters” heavy snowstorms from the North Atlantic
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Maritime Tropical Originate over a warm tropical ocean Warm and moist
Produce thunderstorms in the heat of the day
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Continental Tropical Originate over deserts Hot and dry
Produce tremendous heat waves
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What are the 5 types of air masses?
Continental Arctic, Continental Polar, Maritime Polar, Maritime Tropical, and Continental Tropical
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Fronts
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Fronts Front: The boundary that separates opposing air masses
Characteristics Width: 200 meters to 200 Kilometers Height: up to 5 kilometers Length: up to 2000 kilometers Usually bring precipitation Most common at mid latitudes Where polar and tropical air masses meet
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The boundary that separates opposing air masses
What is a front? The boundary that separates opposing air masses
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Shape of a front The less dense air mass is forced to rise over the denser air mass. This makes the front wedge shaped.
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Cold Front Boundary between an advancing cold air mass and the warmer air mass it is displacing Steep slope Narrow band of precipitation Moves quickly
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Warm Front Warm air displaces cold air Gradual slope Cirrus clouds
Steady rain or snow for extended time Weather warms when it passes
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Occluded Front Occluded: When a cold front catches a warm front
Causes cloudiness and precipitation
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Stationary Fronts Stationary: When a front is not moving
Causes cloudiness and precipitation If stationary too long, flooding may occur
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What happens if a stationary front remains in the same place for too long?
flooding
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