EF3 Tornado — Murray, Oklahoma

2024-04-27 · near Sulphur, Murray, Oklahoma

Event narrative

The Sulphur tornado initially developed in the Chickasaw National Recreation Area to the southwest of Sulphur and produced tree damage as well as damage to one building in the northeast section of the park as the tornado approached Sulphur. The tornado moved into the southern part of Sulphur causing significant damage to a number of homes on Tishomingo Avenue adjacent to the Chickasaw NRA.

The tornado moved northeast through downtown Sulphur destroying or causing extensive damage to numerous businesses and buildings downtown. Many people were trapped and one woman was killed when a building housing a sports lounge collapsed downtown on this Saturday night. Damage was rated EF3 to numerous buildings downtown, as well as to some homes and buildings in neighborhoods across northeast Sulphur as the tornado continues to move northeast through town.

The tornado continued northeast out of Sulphur and damaged another home along Palmer Road in northeastern Murray County. Tree damage was also observed on the county line as the tornado moved from Murray County into Pontotoc County.

Wider weather episode

A widespread, long-duration and historic severe weather and tornado outbreak occurred from the late morning through late evening on the 27th. In all, 32 tornadoes affected portions of the WFO Norman Forecast Area, the third most in a single day during the period of reliable record. This included six significant (EF-2+) tornadoes and one violent (EF-4) tornado that struck Marietta (Love County).

Synoptically, a slow-moving and deep mid/upper-level wave progressed across the Four Corners region during the day. At the surface, an area of low-pressure strengthened/deepened across southwest Kansas, with a trailing dryline extending near and just west of the 100th meridian through much of the day. As ascent overspread this feature, numerous (organized) severe thunderstorms developed across the WFO Norman Forecast Area, even by as early as daybreak/early morning hours. The boundary layer was characterized by strong instability and wind shear, favorable for an organized/supercell storm mode. Initial supercells across western Oklahoma produced a few reports of large hail and the first (brief) tornadoes of the event just after 10 AM. Supercell storm development continued across portions of the area, focusing along an axis from western-north Texas into north-central Oklahoma through much of the afternoon. The first significant (EF-2) tornado of the event impacted the eastern edge of Knox City (Knox County, Texas) just after 3 PM. Through the evening, a quasi-linear convective system (QLCS) organized and swept across much of southern/central Oklahoma and adjacent north Texas. Numerous mesovortex-type tornadoes developed and impacted the aforementioned areas. Ahead of the main convective line, strong warm air advection, driven by an increasing (45-60 knot) low-level jet, promoted the development of pre-frontal/line supercell thunderstorms. Multiple of these storms became strongly tornadic, producing multiple strong and long-tracking tornadoes. This included an EF-2 tornado impacting the western portions of Ardmore, an EF-3 tornado making a direct impact on the historic downtown district and adjacent neighborhoods in Sulphur, an EF-3 tornado traversing western portions of Hughes County, just west of Holdenville, and an EF-4 tornado destroying a Dollar Tree distribution center and nearby large retail stores on the western side of Marietta. The latter three tornadoes resulted in fatalities (1 in Sulphur, 2 near Holdenville and 1 in Marietta) along with additional injuries.

Beyond severe weather outcomes, a significant flash flooding event occurred from the late evening of the 27th through mid-morning of the 28th. The corridor of highest rainfall, with observed 24-hour totals of 5-to-8 inches, occurred across portions of south-central into southeast Oklahoma, on the heels of a cluster of significant tornado impacts earlier in the evening. Additional flooding occurred across far northern Oklahoma (Kay County) during the evening of the 27th.

View location on OpenStreetMap → (34.4740, -96.9920)

Source: NOAA Storm Events Database, event_id 1175817. Narrative written by the NWS forecast office that issued the report.