How do tornadoes form?
The truth is that scientists don’t fully understand how tornadoes form. Typically, tornadoes develop several thousand feet above the earth’s surface inside of a severe rotating thunderstorm. This type of storm is called a supercell thunderstorm. The spinning of these supercell thunderstorms is visible via Doppler radar.
The classic answer — “warm moist Gulf air meets cold Canadian air and dry air from the Rockies” — is a gross oversimplification. Many thunderstorms form under those conditions (near warm fronts, cold fronts and drylines respectively), which never even come close to producing tornadoes. Even when the large-scale environment is extremely favorable for tornadic thunderstorms, as in an SPC “High Risk” outlook, not every thunderstorm spawns a tornado. The truth is that we don’t fully understand. The most destructive and deadly tornadoes occur from supercells — which are rotating thunderstorms with a well-defined radar circulation called a mesocyclone. [Supercells can also produce damaging hail, severe non-tornadic winds, unusually frequent lightning, and flash floods.] Tornado formation is believed to be dictated mainly by things which happen on the storm scale, in and around the mesocyclone. Recent theories and results from the VORTEX program suggest that once a mesocyclone is underway,
