Editing Warm front (section)

{{short description|Boundary of advancing mass of warm air}}
[[File:Warm front.svg|thumb|220px|Illustration of a warm front. The warm air behind the front is slowly overtaking the cold air ahead of the front, which is moving more slowly in the same direction. The warmer air, due to lower density, rises over the colder air as it moves. As a result of its increased altitude, it cools off and its moisture condenses, forming clouds and possibly precipitation.]]
[[File:Warm front symbol.svg|thumb|Symbol commonly used to represent a warm front.]]
A '''warm front''' is a [[weather front|density discontinuity]] located at the leading edge of a homogeneous warm [[air mass]], and is typically located on the equator-facing edge of an isotherm gradient. Warm fronts lie within broader troughs of low pressure than [[cold front]]s, and move more slowly than the cold fronts which usually follow because cold air is denser and less easy to remove from the Earth's surface.<ref name="DR">{{cite web|author=David Roth|date=2006-12-14|title=Unified Surface Analysis Manual|access-date=2010-12-17|publisher=[[Hydrometeorological Prediction Center]]|url= http://www.wpc.ncep.noaa.gov/sfc/UASfcManualVersion1.pdf}}</ref>  This also forces temperature differences across warm fronts to be broader in scale.  
Clouds ahead of the warm front are mostly [[Stratus cloud|stratiform]], and rainfall generally increases as the front approaches. [[Fog]] can also occur preceding a warm frontal passage. Clearing and warming is usually rapid after frontal passage.  If the warm air mass is unstable, thunderstorms may be embedded among the stratiform clouds ahead of the front, and after frontal passage thundershowers may continue.  On [[surface weather analysis|weather maps]], the surface location of a warm front is marked with a red line of semicircles pointing in the direction of travel.<ref name="DR"/>