70% of tornadoes occur in central US
low-lying topography
meeting of air masses creates ideal conditions for thunderstorm formation:
warm, moist air moving up from the Gulf of Mexico
cold, dry air moving down from Canada or out from the Rocky Mountains
high altitude jet stream moving east of >150 mph
all 3 masses are moving in different directions
when they collide, wind-shear can happen
warm, moist air rises, latent heat then releases, and strong updrafts are then created, updrafts sheared and spun by fast-moving cool air and jet stream
spinning motion enhanced by updrafts and downdrafts