.
Effects of Frontal Lifting
on forecasted precipitation

Forecast Tip:
If there is sufficient moisture in the air and a forcing mechanism like a cold front (for example) is approaching the area, then there is an increased probability that precipitation will occur.

Clouds and precipitation are formed by the upward motion of air. Therefore, there must be a mechanism present to lift the air. Fronts often serve as such a mechanism. Air on one side of the front typically blows in a different direction from the wind on the other side, causing the air to converge, or pile up right along the frontal surface.


Since this air has to go somewhere, it rises. As air rises, the moisture in the rising air cools, condenses and forms clouds and precipitation. For example, a cold front lifts warm moist air ahead of it as it advances. The rising air cools and the water vapor condenses out to form clouds, most commonly ahead of and along the cold front (diagram below).


As the cloud droplets grow in size, they begin to fall back to the earth as precipitation. Vigorous upward motions often occur ahead of and along a cold front, resulting in more vertically developed clouds like cumulonimbus clouds, which themselves can produce heavy rains and powerful thunderstorms.

Forecast Tip:
If there is sufficient moisture in the air and a forcing mechanism like a cold front (for example) is approaching the area, then there is an increased probability that precipitation will occur.



Temperatures
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.

moisture