WW2010
University of Illinois

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

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

Tstorm Components
 
  introduction
 
  updrafts/downdrafts
 
  wind shear
 
  outflow phenomena
 
> wall clouds

Wall Clouds
 
  introduction
 
  beneath cb towers
 
  short-lived
 
  cyclic wall clouds
 
> with rotation

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.
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Rotating Wall Clouds
indicative of mesocyclones

Here is another wall cloud on another day, looking north-northeast from about 6 miles away. This wall cloud was rotating, but periodically seemed to become undercut by outflow and lose its rotational characteristics. The storm was severe, and Doppler radar near Norman, Oklahoma, did indicate a mesocyclone, but no tornadoes developed.

[Image: rotating wall cloud (78K)]
Photograph by: Doswell

We have emphasized that many thunderstorms are hybrids and contain characteristics of several of the storm classification groups that we have discussed. These storms will be difficult to warn for. The forecaster needs all the pertinent radar and spotter information that he/she can get to make an appropriate warning decision. In the case of this last storm, a tornado warning is quite probably justified, even though no tornadoes occurred. With some of the weaker wall cloud storms that we have shown, a severe thunderstorm warning likely would suffice.

[Image: another rotating wall cloud (62K)]
Photograph by: Moller

Looking east from about 5 miles away, a furiously rotating wall cloud was moving northeast across the forests east of Logansport, Louisiana. Spotting in the southeast and east U.S. is more difficult because of trees, hills, and typically hazy conditions.

However, the basic building blocks of storms are the same in these areas as they are around the world, although some regional differences do exist in storm structure detail. In fact, the first study of a supercell was from England, with subsequent studies coming from the Soviet Union, Canada and the United States. This storm did produce large hail, but lack of access into the affected forest areas precluded positive identification of a tornado touchdown.



cyclic wall clouds
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Credits and Acknowledgments for WW2010.
Department of Atmospheric Sciences (DAS) at
the University of Illinois at Urbana-Champaign.

Tornadoes