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.
[ [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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warm front — noun count the front edge of a mass of warm air that brings warm weather when it moves into an area. The front edge of a mass of cold air is called a cold front … Usage of the words and phrases in modern English
warm front — n an expression used especially in weather reports meaning the front edge of a mass of warm air ≠ ↑cold front … Dictionary of contemporary English
warm front — warm′ front n. mer a transition zone between a mass of warm air and the colder air it is replacing • Etymology: 1920–25 … From formal English to slang
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
warm front — noun the front of an advancing mass of warmer air • Hypernyms: ↑front * * * noun : the forward boundary of a warm air mass moving to replace a retreating cold air mass see front illustration * * * Meteorol. a transition zone between a mass of… … Useful english dictionary
warm front — UK / US noun [countable] Word forms warm front : singular warm front plural warm fronts science the front edge of a mass of warm air that brings warm weather when it moves into an area. The front edge of a mass of cold air is called a cold front … English dictionary
warm front — A front along which warm air replaces cold air. If the warm air mass progressively passes over ground previously covered by cold air, the front will be a warm front. As this front passes an observer, the heavy stratus type of clouds and any… … Aviation dictionary
warm front — n. a warm front approaches; forms * * * forms a warm front approaches … Combinatory dictionary
warm front — noun A warm front is the trailing edge of a retreating mass of cold air … Wiktionary
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