[1] The most destructive events took place on May 4 when an intense supercell thunderstorm produced a family of 22 tornadoes in central Kansas,[2] one of which inflicted EF5 damage across the small town of Greensburg (with a population of around 1,500).
[3][4] The event was precipitated by a nearly stationary upper-level trough along the Utah–Nevada border with three surface boundaries extending across Kansas, Nebraska, Oklahoma, and Texas.
[4][5] A dry line formed over Kansas, Texas, and the Oklahoma Panhandle late on May 4 and became the focal point for extensive severe thunderstorm development.
The likelihood of widespread severe weather prompted the issuance of a high-risk convective outlook from the Storm Prediction Center.
[1] This resulted from more resilient caps inhibiting thunderstorm development and from the upper-level trough shifting east and weakening.