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

.
From The Developers...

This navigation system remembers the last place you were within a given section. For example, if you were to click on any unhighlighted item in the "Prerelease Info" menu, then click again on the item "ww2010 user's guide", you'll come right back here. Go ahead, try it.


Cyclones and Associated Cold Front
leading edge of colder air mass

The diagram below shows a cyclone complete with warm and cold fronts. The cold front typically extends to the south from the center of low pressure while the warm front extends to the east (ahead of the storm). At low levels, several air masses of distinctly different origin may be found in varying parts of the cyclone. To the east of the cyclone, the moist air mass is moving to the north behind the warm front. The cold front marks the leading edge of a colder and drier air mass. Driven by counterclockwise winds around the center of low pressure (shown by the arrows), the cold air mass is dragged southward by north and westerly winds behind the low.

Clouds and precipitation often develop along and ahead of the cold front as the colder air mass lifts the warm moist air mass ahead of it.



precipitation
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.

Multiple Interfaces