Warm front

A warm front is defined as the leading edge of an advancing mass of warm air; it separates warm air from the colder air ahead. Air masses are large bodies of air with similar properties of temperature and humidity that form over source regions, and the warm air masses behind warm fronts are not only warmer but higher in humidity than the colder air preceding them. Because of a warm air mass’s higher temperature and thus lesser density, mixing between the two air masses is discouraged. Being lighter, the warm air mass is unable to displace the cooler air mass and instead is forced upward along the upper boundary of the colder air in a process known as overrunning. The boundary between the two air masses has a gradual slope of 1:100 and lifting is slow but persistent.

As the air mass rises into regions of lower pressure, it expands and cools. As it cools, water vapor condenses and forms extensive cloud coverage. The first clouds to form along the sloping surface of the cold air are nimbostratus, followed by altostratus, cirrostratus, and cirrus. Once the clouds have thickened to 2,500m from the earth’s surface, rain can begin to fall.

If the air mass is relatively stable, rainfall will increase until the front reaches the location, at which time the clouds can extend all the way to the earth’s surface as fog. Once the front passes, the location experiences quick warming and clearing. If the air mass is unstable, thunderstorms may precede and follow the front.

In the northern hemisphere, a warm front causes a shift of wind from southeast to southwest, and in the southern hemisphere a shift from northeast to northwest. Common characteristics associated with warm fronts include:

On weather maps, the surface location of a warm front is marked with a red line of half circles pointing in the direction of travel. On colored weather maps, warm fronts are illustrated with a solid red line.

ee also

* Cold front
* Pseudo-warm front
* Weather front

References

[ [http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/af/frnts/wfrnt/def.rxml Warm Front: transition zone from cold air to warm air ] ] [ [http://www.ace.mmu.ac.uk/eae/Weather/Older/Warm_Fronts.html Warm Fronts ] ]


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Look at other dictionaries:

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  • warm front — n. Meteorol. the forward edge of an advancing mass of warm air that replaces colder air, usually while causing steady precipitation …   English World dictionary

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