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Severe Weather Training Sessions Hurricane and Extreme Storm Impact Studies
American Meteorological Society's Datastreme Project About River Forecasting
Weather Educational Resources for Teachers About Rainbows
National Weather Service Outreach Site About Lightning
Weather Related Conversion Calculator About Radar and Satellites
UIUC Guide to Meteorology About the Northern Lights (Aurora)
UIUC Cloud Catalog The Beaufort Wind Scale
Plymouth College Cloud Boutique Globe Kids Educational Site
Owlie Skywarn Gives Kids Weather
Safety Tips
Red Cross Educational Disaster Safety Site
El Nino Site

 

Time exposure of the Aurora Borealis November 2001 as seen from Vincennes, Indiana. The Aurora Borealis or more commonly called "Northern Lights" are thought to be the result of high charged solar particles interacting with the Earth's electromagnetic field. Higher than normal solar activity allowed the "Northern Lights" to be seen much further south than normal during October and November 2001. The bright sphere at the lower right hand part of the photograph is actually a full moon and not the sun as it would appear. This photo is courtesy of Sam Sievers, a COOP observer at Vincennes. 

 

Thunderstorm Anvil

Thunderstorm anvils form as relatively strong upper level winds blow the tops of thunderstorms downwind.

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  • Page last modified: 28 -Feb -2006 7:56 PM UTC
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