2013 EF5 tornado in Moore, Oklahoma
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The 2013 Moore tornado was a large and violent EF5 tornado that ravaged Moore, Oklahoma, and adjacent areas on the afternoon of May 20, 2013, with peak winds estimated at , killing 24 people (plus two indirect fatalities) and injuring 212 others. The tornado was part of a larger outbreak from a slow-moving weather system that had produced several other tornadoes across the Great Plains over the previous two days, including five that had struck portions of Central Oklahoma the day prior on May 19.
The tornado touched down just northwest of Newcastle at 2:56 p.m. CDT (19:56 UTC), and quickly became violent, persisting for 39 minutes on a path through a heavily populated section of Moore, causing catastrophic damage of EF4 to EF5 intensity, before dissipating at 3:35 p.m. CDT (20:35 UTC) outside of Moore. The tornado was over across at its peak width.13 The 2013 Moore tornado followed a roughly similar track to the deadlier 1999 Bridge Creek–Moore tornado, which was rated F5; neither of the stricken schools in the area had acquired purpose-built storm shelters in the intervening years.
The tornado caused catastrophic damage around the city of Moore, with 1,150 homes destroyed as a result. Damage estimates ranged up to $2 billion, making it the costliest tornado since the 2011 Joplin tornado. As of 2025, this tornado is the most recent to be rated EF5 officially.
Meteorological synopsis.
On May 20, 2013, a prominent central upper trough moved eastward toward the Central United States, with a lead upper low pivoting over the Dakotas and Upper Midwest region. A Southern stream shortwave trough and a moderately strong polar jet moved east northeastward over the southern Rockies to the southern Great Plains and Ozarks area, with severe thunderstorms forming during the peak hours of heating. With the influence of moderately strong cyclonic flow aloft, the air mass was expected to become unstable across much of the southern Great Plains, Ozarks, and middle Mississippi Valley by the afternoon hours.
Evidence of an unstable air mass included temperatures in the low to mid 80s °F (27–30 °C), dewpoints that ranged in the upper 60s °F (20 °C) to the lower 70s °F (20–22 °C), and CAPE values ranging from 3500 to 5000 J/kg. Deep-layer wind shear speeds of enhanced storm structure and intensity. These were present ahead of a cold front extending from a surface low in the eastern Dakotas, southwestward to near the Kansas City area and western Oklahoma, and ahead of a dry line extending from southwest Oklahoma southward into northwestern and west-central Texas. Outflow remnants from the previous night and the early day convection across the Ozarks and the middle Mississippi Valley were a factor in severe weather development with the most aggressive heating and destabilization on the western edge of this activity across the southern Great Plains and just ahead of a cold front. The National Weather Service office in Norman, Oklahoma had warned as early as May 15 that there would be a possibility of severe weather on May 20.
The most intense severe weather activity was expected to come across the southern Great Plains, specifically Central Oklahoma, during the afternoon hours on that Monday. As such, the Storm Prediction Center issued a moderate risk of severe thunderstorms during the early morning hours of May 20 from southeastern Missouri to north-central Texas. The degree of wind shear, moisture, and instability within the warm sector favored the development of supercells. Very large hail and tornadoes were both expected with these supercells, with the possibility of a few strong tornadoes. The Storm Prediction Center issued a tornado watch at 1:10 p.m. Central Daylight Time (CDT) early that afternoon for the eastern two-thirds of Oklahoma, northwestern Arkansas, and portions of north-central Texas. Given the atmospheric parameters thought to be in place at the time, the Storm Prediction Center inadvertently underestimated the threat of tornadic activity that afternoon; the probability table for the tornado watch – the 191st severe weather watch issued by the guidance center in 2013 – indicated a 40% (or "moderate") probability of two or more tornadoes and a 20% (or "low") probability of one or more tornadoes reaching between EF2 and EF5 intensity within the watch area. The watch did, however, say that "one or two strong tornadoes" were possible.
Development and track.
The thunderstorm that eventually produced the tornado developed less than one hour after the tornado watch was issued, around 2:00 p.m. CDT, across northern Grady County. Its rapid intensification resulted in the National Weather Service Weather Forecast Office in Norman issuing a severe thunderstorm warning for northern Grady, northwestern Cleveland, northern McClain, and southwestern Oklahoma Counties (including southwestern portions of the immediate Oklahoma City area) at 2:12 p.m. CDT. The thunderstorm quickly attained supercell characteristics, with rotation at the mid-levels of the storm's cloud structure becoming apparent even before it was officially classified as severe, due to the sufficient amounts of wind shear present over central Oklahoma.
Due to the expected intensity of the storms, three of the Oklahoma City market's five television news outlets − NBC affiliate KFOR-TV (channel 4), ABC affiliate KOCO-TV (channel 5) and CBS affiliate KWTV (channel 9) − suspended normal programming and went into wall-to-wall weather coverage immediately after the tornado watch went into effect. Fox affiliate KOKH-TV (channel 25) and Telemundo affiliate KTUZ-TV (channel 30) began their coverage as the first severe thunderstorms erupted southwest of the state capital and subsequently began relaying their audio feeds to radio stations throughout central Oklahoma. As the forecast suggested that the most significant severe weather would occur in the mid-afternoon, around the time classes concluded for the day, many worried parents began arriving at schools throughout Moore and south Oklahoma City to pick up their children in advance of the storms.
At 2:40 p.m. CDT, as rotation in the supercell was increasing at the cloud base, a tornado warning was issued for far northeastern Grady, western Cleveland, northern McClain, and southern Oklahoma Counties, as the storm approached the Oklahoma City metropolitan area. The rapid formation of the storm may have been associated with a descending reflectivity core and interplay of complex cell mergers.
Formation and initial intensification.
The tornado touched down at 2:56 p.m. CDT in northwestern McClain County, near Long Drive to the southwest of the North Country Club Road and SH-37 intersection, roughly northwest of downtown Newcastle. Initially a narrow rope-shaped tornado, it first caused EF1 damage to a home and some trees before crossing SH-37 and rapidly intensifying as it struck a semi-rural subdivision, where several homes were destroyed, two of which were leveled at EF4 intensity. At this point, the tornado began to grow rapidly in size over the course of 2 minutes; the rope-like funnel started to swell into a large stovepipe, before maturing further into a barrel shape. A debris ball grew around the funnel itself as it finally evolved into a large, wedge-shaped structure. Slight ground scouring began in this area, and several homes in a subdivision further to the northeast sustained EF3 damage. By 3:01 p.m. CDT, the National Weather Service issued a second, more strongly worded warning for the area: in a severe weather statement updating the existing tornado warning, the Norman forecast office declared a tornado emergency for southern Oklahoma City and Moore as various storm spotters confirmed that the large, violent tornado was approaching the area. The Twin Lakes dual-polarization NEXRAD radar (near Lake Stanley Draper) detected a tornado debris signature one mile in diameter within the accompanying hook echo, as the tornado crossed into portions of south Oklahoma City in northern Cleveland County. The supercell also produced straight-line winds of for at least one mile surrounding the tornadic circulation.
South Oklahoma City.
The tornado maintained at least EF3 intensity as it crossed the Canadian River into Cleveland County and a decommissioned US 62/US 277 bridge was severely damaged; most of this bridge had to be demolished after the tornado ripped part of it from its mount and tossed it across I-44/US 62/SH-37. The tornado then continued moving east-northeastward through the extreme southern portion of Oklahoma City towards Moore, roughly following Southwest 149th Street. At that point, it began to grow rapidly in width, and a second brief area of EF4 damage was noted near South May Avenue, where several homes were leveled, and one was swept clean from its foundation (this home was determined to have been nailed, rather than bolted to its foundation). A vehicle frame, engine block, and various other vehicle parts were found tangled within a grove of completely debarked trees in this area. As the tornado began to cross into south Oklahoma City, a traffic jam had occurred for a stretch of several miles along Santa Fe Avenue, as residents attempted to either escape from or pick up their children at schools located near the tornado's path. As the station's news helicopter was capturing live video of the tornado, then-KWTV chief meteorologist Gary England − upon seeing footage of the backup that was being relayed by pilot Jim Gardner − urged drivers caught in the jam that may have been listening to the station's audio simulcast on area radio outlets to use nearby streets to detour out of the tornado's expected track. The tornado weakened briefly to EF3 strength before re-intensifying to EF4 intensity near Forman Drive, flattening several homes as it moved through mostly rural areas south of Southwest 149th Street. As the tornado struck an oil production site, four oil tanks were blown away, one of which was never found. The others were thrown considerable distances; one was found a mile away.
The tornado maintained its intensity as it struck the Orr Family Farm and the Celestial Acres horse training area, where up to 100 horses were reported killed, some being tossed into and tangled in downed power lines or thrown on top of nearby buildings; several horses that survived the tornado suffered severe injuries, with some being impaled by tree limbs or boards. Every building at Celestial Acres was either leveled or swept away at EF4 intensity, the ground on the property was scoured to bare soil, debris from structures was granulated, and vehicles were thrown and stripped down to their frames. Surveyors noted that based on the contextual damage, the tornado was likely at EF5 intensity in this area, though the construction quality of the affected buildings only permitted an EF4 rating. A 10-ton propane tank on the Orr Farm property was picked up and thrown more than a half-mile through the air by the tornado, and a strip mall near the farm was completely leveled as well. The tornado continued east, heavily scouring an open grassy field before impacting Briarwood Elementary School, which was completely destroyed. The NWS originally rated this damage EF5, but further evaluation and a 2014 study published by the American Meteorological Society revealed evidence of poor construction at the school, and the rating was downgraded to EF4. Remarkably, no fatalities occurred at the school. Two 12,000-gallon water tanks that were also swept off of the Orr Family Farm grounds were thrown into this area; the roof of Briarwood Elementary was struck by one of them − potentially aiding in compromising the building's structural integrity as it bent the steel girders that held up the roof − shortly before the main vortex struck the building, while the other fell onto and destroyed a home a few blocks east of the school. Past Briarwood Elementary, the tornado intensified even further and entered densely populated areas just west of Moore, including the Westmoor subdivision where many well-built, anchor-bolted brick homes were flattened at EF4 intensity, and two were swept clean from their foundations, with damage at those two homes rated EF5.
Moore.
The tornado continued generally northeast at EF4 strength, completely debarking trees and leveling entire neighborhoods as it moved into the western city limits of Moore. Many homes were flattened in neighborhoods to the east of South Santa Fe Avenue. One anchor-bolted home that was reduced to a bare slab in this area was initially rated EF5, but was later downgraded to EF4 as closer inspection of the foundation revealed that the anchor bolts were missing their nuts and washers. The tornado then destroyed Plaza Towers Elementary School at EF4 intensity, where seven children were killed when a cinder block wall collapsed on top of them. More than a dozen homes in a subdivision just to the south of Plaza Towers Elementary