From April 1 to 3, 2024, a significant tornado outbreak,[3] which also included a derecho, affected much of the Midwestern and Southeastern United States.[4][5] The National Weather Service issued dozens of severe thunderstorm and tornado warnings across West Virginia, Kentucky, Tennessee, Ohio, Oklahoma, Kansas, Illinois, Indiana, and Missouri during the event. A total of 32 million people were estimated to be under watches or warnings, and over 150,000 people were estimated to be without power.[6] and 15 people were injured. The event was given an outbreak intensity score of 28 points, ranking it as a significant tornado outbreak, and five people were killed by non-tornadic events as well.[7][8]
On March 28, the Storm Prediction Center (SPC) first delineated a risk of organized severe weather across the Central and Southern Plains, as well as the Mississippi and Ohio River valleys for the beginning of April.[9] By the morning of April 1, a broad category 3/Enhanced risk existed from north-central Texas northeastward toward the Illinois–Indiana border, where widespread supercell thunderstorms were anticipated. The impetus for the severe weather setup came as a large, positively tilted upper-level trough progressed eastward from the Southwestern United States into the Central Plains region.[10] Morning surface observations revealed an area of low pressure over central Kansas, supporting a north-moving warm front to the east into Ohio and a trailing cold front southwestward into Oklahoma and the Texas Panhandle. Meanwhile, an eastward-shifting dry line resided from the Texas Panhandle southward into northern Mexico.[11] Within the warm sector of this low, an unstable environment was expected to develop, with averaged instability values of 2,000–3,000 J/kg, dewpoints in the mid- to upper-60s °F, very strong wind shear throughout the atmosphere, and rapidly cooling temperatures with height. Given these conditions, the SPC upgraded much of the eastern half of Oklahoma and a small section of northern Texas to a category 4/Moderate risk. In this area, the capping inversion aloft was expected to erode throughout the afternoon, giving way to multiple supercells capable of producing large hail in excess of 3 in (7.6 cm). A conditional threat of strong/EF2+ tornadoes existed too as wind shear close to the surface strengthened with time.[12]
Through the afternoon hours, semi-discrete supercells developed across north and central Texas, contributing to widespread reports of large hail the size of baseballs, in addition to hurricane-force wind gusts upwards of 90 mph (140 km/h).[13] Farther to the northeast, isolated severe weather occurred in Oklahoma, though it was curtailed by persistent cloud cover and a broad rain shield across the risk area.[14] Even farther to the northeast, training supercell thunderstorms tracked across the St. Louis metropolitan area, contributing to large hail.[15] By the evening hours, a quasi-linear convective system developed across eastern Oklahoma and progressed toward Missouri and Illinois. As it did so, the squall line interacted with boundaries produced by earlier storms; this resulted in several tornadic circulations along the line.[16] In spite of modest instability, strong vertical wind shear maintained organized convective activity as it spread eastward from southern Illinois and eventually into West Virginia during the pre-dawn and early morning hours.[17][18] Numerous reports of damaging winds were received, including gusts in excess of 90 mph (140 km/h) near Huntington, West Virginia.[19][20] The squall line posthumously met the criteria of a derecho, and post-storm surveys revealed dozens of tornadoes along its track. In particular, 10 tornadoes were confirmed across West Virginia on April 2, the most observed in a single calendar day on record.[5] Convective activity finally lost vigor as it moved toward the West Virginia–Virginia border into a more stable environment.[21]
As the derecho tracked from Missouri to West Virginia early on April 2, another widespread outbreak of severe weather and tornadoes was expected to occur across the broader Ohio River Valley region. On April 1, the SPC issued a category 4/Moderate risk across much of Ohio and adjacent portions of surrounding states. Despite questions about the influence of widespread morning thunderstorms, forecasters felt there was sufficient confidence that the atmosphere would recover over subsequent hours, contributing to discrete or clusters of storms capable of producing damaging winds, large hail, and multiple significant tornadoes.[22] By the afternoon hours of April 2, forecasters expressed concern that morning convection would stunt the degree of destabilization across portions of the risk area, particularly in Ohio. Farther to the west, an environment characterized by surface temperatures of in the low- to mid-70s °F, dewpoints between 65–70 °F (18–21 °C), and strong vertical wind shear was still expected to promote a substantiative risk for strong tornadoes.[23] Storms across southern Indiana and western Kentucky initially struggled to intensify during the afternoon,[24] but they eventually matured into tornado-producing supercells as they continued eastward into western Ohio.[25] As convective activity to the north continued eastward into a drier and more stable environment,[26] a cluster of storms developed farther south across Alabama and Georgia, contributing to additional tornadoes.[27][28] Into April 3, additional severe weather occurred along frontal boundaries from Florida to Virginia before activity pushed offshore.[29][30]
This strong tornado began along the north side of SR 265/SR 62 west of Watson, Indiana in Clark County. It moved eastward, uprooting trees and damaging an outbuilding at EF0 strength. The tornado then quickly intensified to EF1 strength as it crossed SR 62 and moved through Watson. It knocked over three tractor trailers on SR 62 and uprooted some trees. After uprooting additional trees and damaging two homes and an outbuilding, the tornado moved through the neighborhood of Brookhollow in the far northern part of Jeffersonville. In Brookhollow, many garage doors were blown out, windows were broken, brick facade crumbled, trees were uprooted, and large sections of roofs were blown off structures. Many boards were impaled and driven more than a foot into the ground with others being impaled into homes. A large metal building also had portions of its walls removed. The tornado then crossed SR 265 and struck an industrial business at the International Drive/Old Salem Road interchange. The building had parts of its roof section pulled and twisted and a 5,000 lb (2,300 kg) salt pod was lifted up over a 4 ft (1.2 m) concrete barrier and thrown down a hill approximately 40 yd (37 m). The tornado then crossed SR 265 again and broke windows and peeled metal roofing off of more homes in the northern part of Utica before beginning an erratic eastward movement crossing the Ohio River into Kentucky.[46][94]
As it entered Jefferson County, the tornado widened and reached its peak intensity of EF2 as it moved into Prospect and struck the Beechland Beach neighborhood. Three well-built two-story homes suffered significant roof damage, had broken windows, and had air conditioner units twisted and torn from the sides of them. Another home suffered a collapsed exterior wall, and three large pin oak trees were snapped. Continuing to move erratically eastward, the tornado weakened but reached its maximum width as it moved through Hays Kennedy Park and entered the neighborhood of The Sutherlands at high-end EF1 intensity. Numerous homes suffered roof damage, power lines were downed, power poles were snapped, and trees were uprooted. One homeowner was trapped in the basement of his home when a tree fell on his home; he had to be freed by his neighbors. Nearby, a 7 ft (2.1 m) section of a locust tree was torn off, thrown 20 yd (18 m), and impaled about 4 ft (1.2 m) into the ground. A personal weather station on the fence at a home on the edge of the tornado's path recorded a wind gust of 79 mph (127 km/h). The tornado then crossed US 42 and entered the Hunting Creek neighborhood, where more trees were uprooted and more roof damage was dealt to homes, including two homes that suffered total roofing loss; this damage was rated low-end EF2 while the rest of the peak damage received an EF1 rating. The tornado then exited Hunting Creek and crossed into Oldham County as it entered Hidden Creek at a weaker low-end EF1 intensity. Trees were uprooted, barns took damage to their overhead doors and sheet metal, and some homes incurred roof damage. The tornado finally exited Prospect, weakened to EF0 strength as it crossed KY 1694, and turned northeast, striking the southern portion of a golf course, uprooting trees and damaging barns. The tornado then lifted northeast of the golf course as it crossed KY 329/KY 1694 near Brownsboro as the EF2 Buckner tornado was forming to the north.[46][94]
The tornado was on the ground for 14 minutes, traveled 11.59 mi (18.65 km), and reached a peak width of 450 yd (410 m). There were 22 injuries in Jefferson County.[46][94]
Heavy flooding in the Midwest was observed in the days leading up to the outbreak, mainly March 31. Many areas of Ohio, Kentucky, Indiana and West Virginia were put on flood watches and flash flood warnings.[119] Ground-to-cloud lightning was observed throughout the entire outbreak. In Carthage, Missouri, which is northeast of Joplin, straight-line wind damage was reported. Winds gusted up to 100 mph (160 km/h) during that event. Power poles were broken, and trees were snapped as a direct result of these storms. Ground scouring was also observed in parts of Central Oklahoma. In West Virginia, there were dozens of reports of straight-line wind damage along with the tornadoes. A wind gust of 92 mph (148 km/h) was recorded at Tri-State Airport in Huntington, West Virginia, which set an all-time record for that station.[120][5] Heavy snowfall also affected the Midwest, with up to 17 in (43 cm) of snow in Wisconsin.[121]
The University of Kentucky campus in Lexington suffered minor damage from high winds, and afternoon classes and on-campus activities were canceled. The Scioto Audubon Metro Park was completely flooded.[122]
Severe storms across the Northeastern United States on April 3 produced a daily rainfall record of 1.75 in (44 mm) of precipitation at LaGuardia Airport in New York City, with even more rain in Newark, New Jersey.[123] Winds in Central Park reached 59 mph (95 km/h).[124] Lightning also struck the Statue of Liberty during the storms, resulting in viral social media attention.[125] Two Major League Baseball games at Citi Field were postponed during the storm.[126] On April 2, two people were fatally crushed by fallen trees in Pennsylvania. Another fatality occurred in New York on April 3 due to downed trees.[123] Further north, up to 21.5 in (55 cm) of snow fell in Northern New England, with over 600,000 customers losing power.[127]
Over 250,000 people were left without power in the wake of the storm; with many of those outages in West Virginia.[128] At around 4:10 pm on April 2, the state of Kentucky issued a state of emergency.[129][130] West Virginia also declared a state of emergency for 21 counties.[131]
The tornado outbreak was historic in West Virginia according to the National Weather Service. Their Charleston office stated that "The 17 confirmed tornadoes are the most tornadoes for any calendar day and event on record for the NWS Charleston County Warning Area. The previous record was 6 tornadoes on April 4, 1974. To further put this number into perspective, the previous record number of tornadoes for an entire calendar year over the NWS Charleston County Warning Area was 11 set in 1980, and it took 7 different days with tornadoes to reach that number."[5]
Ten tornadoes occurred in West Virginia; which also set a state record for the most tornadoes confirmed in a single day. The previous record was seven; set on both April 4, 1974 and June 2, 1998.[131]
The Storm Prediction Center said this storm system was significant enough to be classified as a Derecho event: a type of severe weather event defined by a bowing line of damaging winds over a far distance.
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