- Generated in regions of already severe thunderstorms
- Two prime factors for initiation: topography, local climate
- Created over areas undisturbed by mountains
- Very common in Midwestern US – “Tornado Alley” (TX, OK, KS, NB, IA)
Formation
- Average dimensions: width – 75 yards; track length – 1-4 miles; time on ground – 5 min; forward speed – 25 mph
- Timing – spring to summer; late afternoon to late evening (time of maximum local ground heating)
- Structure
- Combination of opposing wind patterns
- High level, relatively dry/cooler winds from west
- Lower level, warm/wet winds from east (originating in the Gulf of Mexico)
- Rollers – winds form cyclonic rotation parallel to the ground
- Large thunderstorms pull warmer air upward from low levels; warm/wet air provides energy for storm
- Large updrafts can cause a roller to tip into a vertical position
- Tornado is born upon touchdown with ground
- Large storms can produce more than one tornado – called “families” or “swams”
- Large tornado swarm in 1974; caused damage in 13 states from AL to OH; 148 tornadoes in ~16 hours; 307 killed, 6,000+ injured and $600 mil in damage
- Combination of opposing wind patterns
- Severe pressure drops
- Inside a twister can be as low as 3″ Hg
- For comparison: average daily pressure is ~31-32″ Hg; large thunderstorm can be as low as 27″ Hg
- Movement
- Track direction generally SW to NE
- Combination of prevailing wind direction from west and the counterclockwise rotation of tornado










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