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The region of the U.S. between the Rockies and the appalachians sees a high frequency of tornadoes because of its ideal climatic setup. In the spring, storm systems cause warm, moist air from the Gulf of Mexico to collide with cool air from Canada and sometimes dry air from the Rockies for events further west, resulting in the formation of strong thunderstorms. About a mile off the ground a layer of stable air holds thunderstorm activity back, allowing instability to build underneath it. As a result when the storm break through the cap the instability will be enormous, leading to explosively powerful thunderstorms. At the same time wind speed and direction varies with altitude, which sets these storms rotating and also strengthens the updraft. This rotation combined with strong thunderstorm updrafts can then produce tornadoes.

Additionally, the National Weather Service is very diligent in surveying areas hit by tornadoes, meaning that it records as many tornadoes as it can. Most countries do not have such agencies, and so many tornadoes that occur are never recorded.

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