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Where air masses converge, they form boundaries called fronts. Fronts are identified by a change of temperature based upon their motion. With a cold front, a colder air mass is replacing a warmer air mass. A warm front is the opposite when warm air replaces cold air.
Weather fronts mark the boundary between two different air masses, which often have contrasting properties.
Warm fronts are associated with a frontal inversion (the warmer air overruns the colder air). Warm fronts typically produce less violent weather than cold fronts. Warm fronts are associated with areas of gentle ascent (i.e. stratiform clouds and precipitation).
Weather fronts. Weather fronts mark the boundary or transition zone between two air masses and have an important impact upon the weather.
A weather front is a transition zone between two different air masses at the Earths surface. Each air mass has unique temperature and humidity characteristics. Often there is turbulence at a front, which is the borderline where two different air masses come together.
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