WW2010
University of Illinois

WW2010
 
welcome
 
online guides
 
archives
 
educational cd-rom
 
current weather
 
about ww2010
 
index

Online Guides
 
introduction
 
meteorology
 
remote sensing
 
reading maps
 
projects, activities

Meteorology
 
introduction
 
air masses, fronts
 
clouds, precipitation
 
el nino
 
forces, winds
 
hurricanes
 
hydrologic cycle
 
light, optics
 
midlatitude cyclones
 
severe storms
 
weather forecasting

Air Masses, Fronts
 
introduction
 
air masses
 
fronts
 
advection

Fronts
 
introduction
 
stationary front
 
cold front
 
warm front
 
occluded front
 
dry line

Warm Front
 
definition
 
wind shift
 
higher dew points
 
cyclones
 
precipitation

User Interface
 
graphics
text

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Warm Front
transition zone from cold air to warm air

A warm front is defined as the transition zone where a warm air mass is replacing a cold air mass. Warm fronts generally move from southwest to northeast and the air behind a warm front is warmer and more moist than the air ahead of it. When a warm front passes through, the air becomes noticeably warmer and more humid than it was before.

Symbolically, a warm front is represented by a solid line with semicircles pointing towards the colder air and in the direction of movement. On colored weather maps, a warm front is drawn with a solid red line.

There is typically a noticeable temperature change from one side of the warm front to the other. In the map of surface temperatures below, the station north of the front reported a temperature of 53 degrees Fahrenheit while a short distance behind the front, the temperature increased to 71 degrees. An abrupt temperature change over a short distance is a good indication that a front is located somewhere in between.

If warmer air is replacing colder air, then the front should be analyzed as a warm front. If colder air is replacing warmer air, then the front should be analyzed as a cold front. Common characteristics associated with warm fronts have been listed in the table below.

Before Passing While Passing After Passing
Winds south-southeast variable south-southwest
Temperature cool-cold, slow warming steady rise warmer, then steady
Pressure usually falling leveling off slight rise, followed by fall
Clouds in this order: Ci, Cs, As, Ns, St, and fog; occasionally Cb in summer stratus-type clearing with scattered Sc; occasionally Cb in summer
Precipitation light-to-moderate rain, snow, sleet, or drizzle drizzle or none usually none, sometimes light rain or showers
Visibility poor poor, but improving fair in haze
Dew Point steady rise steady rise, then steady
Table adapted from: Ahrens, (1994)



Cold Front
Terms for using data resources. CD-ROM available.
Credits and Acknowledgments for WW2010.
Department of Atmospheric Sciences (DAS) at
the University of Illinois at Urbana-Champaign.

wind shift