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1991 Andover tornado

F5 tornado in 1991

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Through Tornado and Great Plains

The tornado first touched down near Clearwater, moving northeast while retaining F0 and F1 intensity. The tornado rapidly intensified as it approached Haysville, reaching F3 intensity as it directly impacted the town. After leaving Haysville in ruins, the tornado struck several residential subdivisions in eastern Wichita, where four people were killed. The tornado then tracked across the McConnell Air Force Base, becoming violent shortly before hitting the tarmac. At this location, the tornado narrowly avoided striking ten Rockwell B-1 Lancers, two of which were equipped with nuclear warheads. The tornado then strengthened, reaching F5 intensity for the first time as it entered Andover. A mobile home park located in the town was obliterated, and thirteen people were killed; 165 more were injured as the park was torn apart in winds that were greater than 260 miles per hour (420 km/h). The tornado continued to heavily damage Andover before beginning to weaken after leaving the town. The tornado then struck an oil field, lofting a large oil tank over 0.8 miles (1.3 km) away. A short time later, the tornado dissipated, tracking a total of 46 miles (74 km) over a period spanning almost an hour and a half.

The tornado killed 17 people and produced damage that was rated as F5 by National Weather Service; "F5" is the highest rating a tornado can receive on the Fujita scale.

Meteorological synopsis

On April 25, 1991, the National Weather Service issued a warning of an impending weather system, noting that computer models were "indicating this to be a very significant severe weather producer with tornadoes occurring across the Central/Southern Plains." On the morning of April 26, the organization delineated a High risk of severe weather across the Great Plains. A southeast-tilted trough existed across the Southwestern United States that morning, and a distinct jet streak, or a region of enhanced winds at the base of the trough, on the order of 75–85 kn (85–100 mph; 140–155 km/h) was progressing northeast toward the Plains. Through the morning, an 850 mb or approximately 5,000 ft (1,525 m) low-level jet of up to 60 kn (70 mph; 110 km/h) overspread regions from south-central Kansas northward into eastern Nebraska. A surface low-pressure area existed over southwestern Nebraska, supporting a dry line southward into Texas and a warm front southeastward across eastern sections of Kansas and Oklahoma.

In the unstable atmosphere between those two boundaries, surface dewpoints rose above 60 °F (15 °C). Abundant sunshine contributed to destabilization as lifted indices topped -12 from central Oklahoma into central Kansas and convective available potential energy reached in excess of 4,000 J/kg. A minimal capping inversion existed across Oklahoma even during the morning l, and tornado-producing storms first developed across western Oklahoma around sunrise. These storms weakened as they moved northeast into Kansas. Back to the west, the dryline progressed rapidly eastward but began to slow precipitously during the afternoon. Attempts at thunderstorm development along this feature initially failed. At 17:10 UTC (12:20 p.m. CDT), the National Weather Service issued a particularly dangerous situation tornado watch, warning of the potential for multiple strong to violent tornadoes.

Despite early failure at convective initiation, supercell thunderstorms rapidly erupted along the dryline during the afternoon as the jet streak propagated into the Great Plains, resulting in a regional outbreak of tornadoes stretching from Texas to Iowa. Violent tornadoes were concentrated in southern Kansas and Oklahoma, although tornadoes were also observed in Iowa, Texas, and Nebraska.

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