WW2010
University of Illinois

WW2010
 
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Online Guides
 
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> meteorology
 
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Meteorology
 
  introduction
 
  air masses, fronts
 
  clouds, precipitation
 
  el nino
 
  forces, winds
 
  hurricanes
 
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  light, optics
 
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> severe storms
 
  weather forecasting

Severe Storms
 
  introduction
 
  dangers of t-storms
 
  types of t-storms
 
  tstorm components
 
  tornadoes
 
> modeling

Modeling
 
  introduction
 
  supercells
 
  convective lines
 
> forecasting

Forecasting
 
  introduction
 
  forecast matrix
 
  parameters
 
> ncsa access article

NCSA Access Article
 
  page 1
 
  figure 1
 
> page 2
 
  figure 2
 
  page 3
 
  figure 3
 
  page 4

User Interface
 
  graphics
> text

NOTE: We've guessed that you're not using a client that supports colored tables and have tried to compensate. Low graphics mode looks much better on clients that do... we recommend switching to Netscape 3.0 or Microsoft Internet Explorer.
. Access Feature: Stormy Weather
 
[Image: ] Droegemeier has been simulating severe storms for 15 years, first as a graduate student working with Robert Wilhelmson at the University of Illinois at Urbana-Champaign (and now also at NCSA), where he reproduced storms to understand how they formed, and later as a professor at the University of Oklahoma, where he built forecasting models and studies of the dynamics and predictability of storms. In 1989, he and an Oklahoma colleague, Doug Lilly, were awarded an 11-year grant from the National Science Foundation to establish a Science and Technology Center that would go beyond predicting the conditions favorable to the formation of severe storms to predicting when and where a storm will strike. The result was ARPS. 

ARPS was designed for all types of local high-impact weather but has been tested most extensively on the so-called supercell storms: the towering thunderstorms that darken skies in the spring and can unleash within their one- to two-hour lifespans the energy equivalent to several atomic bombs. "Supercell storms are among the most menacing weather events," says Droegemeier, "and are difficult to predict with computer models." 

(Figure 2)

Why? Meteorologists have known since the 1950s that thunderstorms form where cold, dry air overlies warm, moist air. Some slight instability shoves the warm air upwards, triggering a cycle of updrafts and downdrafts that erupt into storms. A hitch has been identifying these triggers. A mountain range will do it, but so will small differences in vegetation and soil moisture. Then there's predicting the motion and decay of the storms once they form. 

[Image: 2 ]



figure 1
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.

figure 2