Cold front

leading edge of a cooler mass of air From Wikipedia, the free encyclopedia

Cold front
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A cold front is a meteorological word describing the movement of a cooler air mass into an area of warmer air.[1] The air with greater density moves under the less dense warmer air, lifting it, which can create a line of showers and thunderstorms, or a squall line to form when there is sufficient moisture. This upward motion causes lowered pressure along the cold front.

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Cold front interaction with the warmer air.
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Cold front symbol: a blue line with triangles pointing in its movement direction.

On weather maps, the surface position of the cold front is marked with the symbol of a blue line of triangles or spikes pointing in the direction of its movement. Cold fronts can also move up to twice as fast as warm fronts.

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Precipitation

Rain, snow, hail, and other forms of precipitation can happen with cold fronts.[2]

Effects

Cold fronts can bring dry and colder air behind it.[3] Temperatures can drop to 15 °F behind cold fronts, and it can get very windy.

References

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