A. Thunderstorms

Life Cycle of an Air-Mass T'Storm

Lightning: flashes of light resulting from electrical discharges within the cloud (the majority of strikes), between the cloud and the ground (~20% of strikes), from one cloud to another, or from a cloud to the surrounding air

"Thunder" - results from the expansion of suddenly heated air, which sends out shock waves (the air is heated by the lightning - 15,000-30,0000C

"Hail" - forms within cumulonimbus clouds when raindrops are repeatedly carried above and below the freezing level - layers of ice are added until it becomes too heavy and can no longer be supported by the updrafts


Synoptic Situation Most Favorable for Development of Severe T'Storms



B. Tornadoes

"Fujita Scale" - based on wind speed and property damage; F0-F5                                   
Average Annual Tornado Incidence (per 10,000 square miles)                                     
Average # of Tornadoes and Tornado Days Each Month (27-year period)
 

Tornado Formation: