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The El Reno area on May 24, 2011, had all the ingredients. The atmosphere was incredibly unstable, with a large amount of available convective potential energy (CAPE). CAPE is a measure of the amount of energy available for a thunderstorm to develop. The higher the CAPE, the more intense the storm can be. There was also strong wind shear, providing the necessary rotation. A dryline, a boundary between dry air and moist air, acted as the trigger, sparking the initiation of several supercells, including the one that spawned the infamous El Reno tornado. The combination of high CAPE and strong wind shear created a highly favorable environment for tornadogenesis.
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