During a 4-day period from April 25-28, 2011, more than 200 tornadoes occurred in a five southeastern states.
Debris cleanup in Tuscaloosa alone cost $100 million.The thunderstorm system that created this EF-4 began in Mississippi. Conditions were similar on April 26, with a predicted likelihood of severe thunderstorms, including an extended threat of strong to violent long-track tornadoes throughout the afternoon and evening hours; mixed-layer CAPEvalues were forecast to be aro… East of Cordova, the tornado crossed the The tornado then crossed the Mulberry Fork for the fourth time and moved into This tornado was on the ground for two hours and sixteen minutes, tracking for 127.8 miles (205.7 km) across seven counties. An EF3 tornado caused major damage to homes in From the late morning to the early afternoon, another squall line moved through northern parts of Mississippi and Alabama as high wind shear and low-level moisture persisted. The outbreak produced an EF4 tornado that tore through the St. Louis metropolitan area. So, this supercell existed for about 7 hours and 24 minutes, and traveled approximately 380 miles producing several strong to violent tornadoes along the way. Further details may exist on the The tornado continued into southeastern Kingfisher County.The tornado entered far southeast Kingfisher County before moving into Logan County. Finally, the tornado dissipated northeast of Guthrie with some minor tree damage. April 24 2011- Ralph Minor of Colorado surveys the damage of his nephew's home along Bonniebrook Drive in Maryland Heights Saturday afternoon. Significant wind damage began in southeast Missouri, where estimated 70-75 mph gusts occurred near Marble Hill (west of Cape Girardeau). It was part of the tornado outbreak sequence of April 19–24, 2011. More widespread EF-4 damage was seen west and north of Piedmont. The estimated peak winds were denoted as “greater than 210 mph”This tornado began very close to the Caddo/Canadian County border and quickly became a strong/violent tornado. The tornado killed 20 people and injured hundreds more along its 57-mile (92 km) path across Catoosa, Hamilton, Bradley, Polk and McMinn counties. The 2011 St. Louis tornado was a storm that struck the St. Louis metropolitan area on April 22, 2011. Prior to the spring of 2011, the record number of tornadoes in a single month was 542, set in May 2004, while the record for April was only 267. It was rated as a low-end EF4 with winds of 170 mph (270 km/h). The outbreak of severe weather and tornadoes led to 43 deaths in the Southern United States. Otherwise, severe thunderstorms are possible for parts of the Northeast today, including the New York City area. The tornado was given a rating of EF4 with winds ranging from 175–190 mph (282–306 km/h). Widespread EF-3, occasional EF-4 damage occurred between El Reno and Piedmont. Between April 25 and 28, the outbreak violently struck the southeastern United States, resulting in roughly $11 billion in damages and leaving an estimated 321 people dead.Until April 2011, three years had passed without a single EF-5 tornado—the strongest rating on the The outbreak challenged and surpassed the records set by almost all previous tornado events, ranking as one of the deadliest and most expensive meteorological disasters on record. It affected the Midwest and Southern United States. The tornado and severe storm warnings issued by the National Weather Service in Huntsville on April 27, 2011. Later that morning, the SPC even increased the probability for tornadoes to 45 percent along a corridor from During the early morning hours, a cold front with several embedded low pressure areas extended from east A majority of the tornadoes embedded in this initial squall line were weak, though several were strong and as such caused significant damage. The 2011 Hackleburg–Phil Campbell tornado was an extremely violent and long-tracked EF5 wedge tornado that devastated several towns in rural northern Alabama, before tearing through the northern suburbs of Huntsville and causing damage in rural portions of southern Tennessee on the afternoon and early evening of Wednesday, April 27, 2011. However, EF-3 damage occurred just over the Kingfisher county border, debarking trees and significantly damaging buildings. As the low formed across Texas and deepened while moving east, a tightening pressure gradient force further strengthened the low-level jet, therefore creating a broad warm sector across the southeastern states. Monetary damage estimates were not available.Genesis and maintenance of a long-track EF5 tornado embedded within a supercell thunderstorm by Leigh OrfDid you enjoy reading about this event?
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