WW2010
University of Illinois

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

About WW2010
 
welcome
 
history
 
publications
 
user's guide
 
updates
 
acknowledgments
 
terms for data use
 
clients & cookies

User's Guide
 
project summary
 
content resources
 
core technologies

Core Technologies
 
overview
 
efficient navigation
 
multiple interfaces

Efficient Navigation
 
introduction
 
example: cold fronts

Example: Cold Fronts
 
definition
 
precipitation
 
cyclones

User Interface
 
graphics
text

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From The Developers...

This opens up an additional menu of cold front related topics. So the current page is now "definition" within "Example: Cold Fronts". The items available in the "Example: Cold Fronts" menu include a definition (current page), details about cold fronts and precipitation, plus the importance of cold fronts in cyclones.


Cold Front
transition from warm air to cold air

A cold front is defined as the transition zone where a cold air mass is replacing a warmer air mass. The air behind a cold front is colder and generally drier than the air ahead of it. In the picture below, temperatures ahead of the cold front are 55 and 62 degrees while behind the front temperatures are lower, 31 and 28.

If you were standing outside and a cold front passed through, the air would become cooler and drier than it was before. Occasionally, the temperature can drop as much as 15 degrees in an hour after a cold front comes through.

Symbolically, a cold front is represented by a solid blue line with triangles along the front pointing towards warmer air. The triangles indicate the direction in which the front is moving. On most weather maps however, a cold front is represented by simply a solid blue line.



Efficient Navigation
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.

precipitation