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Chapter 25 Weather. Section 2 Fronts Notes 25-2. Fronts. When two unlike air masses meet, density keeps them separate Warm air is less dense than cold air Front is made between the two air masses Changes in the middle latitude weather takes place along fronts
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Chapter 25Weather Section 2 Fronts Notes 25-2
Fronts • When two unlike air masses meet, density keeps them separate • Warm air is less dense than cold air • Front is made between the two air masses • Changes in the middle latitude weather takes place along fronts • Can be from 100’s of km long to 1000’s of km long • There are no fronts in the tropics • Air is all the same
Types of Fronts • Cold front: cold air over takes warm air • Warm air is lifted by cold air • Warm, moist air will form clouds • Fast moving cold front • Large cumulus or cumulonimbus clouds • Storms are short and violent • Squall line: long line of heavy thunderstorms • Will form ahead of front
Types of Fronts • Cold Front: • Slow moving front • Lifts the air slower • Produces less cloudiness and lighter precipitation
Types of Fronts • Warm Front: • Warm air overtakes a cooler air mass • Warm air rises over cool air • Slope is gradual • Clouds may extend far ahead of the base of the front
Types of Fronts • Warm Front: • Types of clouds • Cirrus clouds = beginning of front • Cirrostratus clouds = next • Altostratus clouds = next • Low stratus clouds = next • Nimbostratus clouds = at base of front • Produces precip. over a large area • Could be violent if the warm air is very moist
Types of Fronts • Stationary Front: • Front that does not move • When two air masses meet and neither can be displaced • Air masses move parallel to each other • Weather is similar to a warm front
Types of Fronts • Occluded Front: • Fast moving cold front overtakes a warm front • Lifts warm off the ground • Cold front comes up to the cold air replacing the warm that just went up into the sky • Warm air becomes secluded above the cold air