2003 Moore-Choctaw tornado
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| Meteorological history | |
|---|---|
| Duration | 39 minutes |
| Date | May 8, 2003 |
| Formed | May 24, 2011, 5:26 p.m. CDT (UTC−05:00) |
| Dissipated | May 24, 2011, 6:05 p.m. CDT (UTC–05:00) |
| EF4 tornado | |
| on the Enhanced Fujita scale | |
| Highest winds | 200 mph (320 km/h) |
| Overall effects | |
| Fatalities | 0 |
| Injuries | 61 |
| Damage | $370.5 million (2003 USD) |
| Areas affected | Cullman County, Morgan County and Marshall County |
| Script error: The function "split" does not exist. IBTrACS | |
Part of the Tornado outbreak sequence of May 2003 and Tornadoes of 2003 | |
Meteorological synopsis
On May 21, a small system of thunderstorms developed in Brown County, Kansas, while another system formed to the southeast of Emporia, Kansas. The Brown county system spawned a brief tornado over Topeka, Kansas, causing minor damage. This system also caused significant damage in Oskaloosa, Kansas, and other communities. Meanwhile, the Emporia system spawned an EF3 tornado that struck Reading, Kansas; one person was killed, several others were injured, and at least 20 houses were destroyed.[1] These two systems developed several other tornadoes throughout the evening.[2]
A moderate risk of severe weather was issued for much of the Midwest, as well as further south to Oklahoma for May 22. The first tornadic supercell developed in the mid-afternoon hours over the western Twin Cities in Minnesota, and caused moderate damage in the Minneapolis area.[3] Shortly thereafter, an intense tornado crept towards Harmony, Minnesota, prompting the National Weather Service to issue the first tornado emergency of the outbreak. Late that afternoon, a large, intense EF5 multiple-vortex tornado left catastrophic destruction in Joplin, Missouri. Causing 158 fatalities, it was the deadliest single tornado in the U.S. since at least 1947.
On May 24, a high risk of severe weather was issued for parts of south-central Kansas, central and eastern Oklahoma, and extreme north-central Texas; a moderate risk was issued for surrounding areas in those three states plus northwestern Arkansas and southwestern Missouri. Throughout this region, strong to violent tornadoes were considered to be highly probable for three reasons: (1) the stationary front was expected to maintain its position over the region, (2) wind shear was expected to greatly increase, and (3) these elements would be associated with an incoming trough. Late that morning, the tornado threat increased to 45%, a rare occurrence matching the widespread April 27 outbreak.[4] At 12:50 p.m. CDT, the SPC issued a Particularly Dangerous Situation (PDS) tornado watch for parts of central Oklahoma, including Oklahoma City and northern Texas, in effect until 10:00 p.m. CDT.[5] Numerous tornadoes touched down in several regions, with the first activity being in western Oklahoma that afternoon where several very intense tornadoes developed, which included the Goldsby tornado.
Tornado summary
The tornado touched down west of Bradley, causing EF0 to EF1 tree damage as it crossed SH-19. Large tree branches were broken as the tornado moved to the northeast, passing to the northeast of Bradley. The tornado would first produce EF1 damage as it moved across the Washita River, where it snapped large trees. West of Ash Road, the tornado would reach EF2 intensity as it continued to damage trees in largely unpopulated areas between Alex and Bradley. The tornado destroyed a fence as it crossed the intersection of River Road and Mellegaard Road, shortly before reaching EF3 intensity as it debarked trees and widened. A manufactured home on the McClain County Line was completely destroyed at EF2 intensity; the tornado was estimated to have had 150 miles per hour (240 km/h) at this point in its life.[6]
The tornado then reached EF4 strength as it crossed SH-76, leveling and sweeping away several well-built homes. Vehicles were thrown long distances and mangled almost beyond recognition nearby. A home located on 170th Street sustained low-end EF4 damage as it took a direct hit from the tornado, and nearby trees were completely debarked, with some being uprooted from the ground. Another home on the nearby Rockwell Avenue was also destroyed; damage at the location was given a low-end EF4 rating due to construction flaws.[6]
The tornado weakened and narrowed as it crossed CR 410, with EF2 to EF3-strength damage occurring in that area. The tornado re-intensified to EF4 strength further to the northeast as it passed between Dibble and Washington. Numerous well-built homes were leveled in that area, and some were swept completely away. Unusual cycloidal debris impact scars were noted in open fields as well. One well-built home in this area with numerous anchor bolts was reduced to a bare slab, though a metal fence immediately next to the house remained standing and grass on the property was not scoured. Another home that was reduced to a bare slab in this area had anchor bolts spaced every two feet (well above the standard of anchoring required for an EF5 rating), though a closer inspection of the home site revealed that a large mobile home frame had smashed into the house during the tornado, and a Jacuzzi found in the rubble behind the house was still in usable condition.
Due to these contextual discrepancies, damage in this area was rated high-end EF4 rather than EF5.[7][8] The tornado curved sharply to the north and weakened to EF3 strength as it continued north of Washington, though one final area of EF4 damage occurred southwest of Goldsby as a large, well-built home was completely swept away with only the slab remaining, and large metal storage tanks behind the house were tossed. This home was specifically engineered to be tornado resistant, though close inspection of the foundation revealed that some of the anchor bolt washers were missing, and the ones that were present were slightly too small, preventing a rating higher than EF4. Further to the north, minor EF0 damage occurred near David Jay Perry Airport before the tornado dissipated. Large amounts of debris from this tornado reportedly fell from the sky in Norman.[7]
Overall, the tornado was on the ground for 23 miles (37 km). 61 people were injured, though no fatalities occurred. Despite the presence of multiple well-built, anchor-bolted homes being swept completely away along the path, the tornado was not rated EF5 due to several contextual discrepancies and minor anchoring flaws. A high-end EF4 rating was applied as a result. Despite this, much like the Chickasha–Blanchard tornado, the EF4 rating is disputed, and the tornado is suspected by some in the academic sector to have been an EF5.[7][9]
Aftermath
One home in Goldsby was destroyed, and sixteen others sustained damage to varying degrees.[10] The Goldsby Baptist Church would end up being used as a shelter in the immediate aftermath of the tornado.[11]
See also
Notes and footnotes
Notes
Footnotes
This article "2003 Moore-Choctaw tornado" is from Wikipedia. The list of its authors can be seen in its historical and/or the page Edithistory:2003 Moore-Choctaw tornado. Articles copied from Draft Namespace on Wikipedia could be seen on the Draft Namespace of Wikipedia and not main one.
- ↑ "One Killed In Reading, KS Tornado". KAKE. Associated Press. May 21, 2011. Archived from the original on May 23, 2011. Retrieved May 22, 2011. Unknown parameter
|url-status=ignored (help) - ↑ "Storm Reports for May 21, 2011". Storm Prediction Center. National Oceanic and Atmospheric Administration. May 21, 2011. Archived from the original on May 25, 2011. Retrieved May 22, 2011. Unknown parameter
|url-status=ignored (help) - ↑ "Storm Reports for May 22, 2011". Storm Prediction Center. National Oceanic and Atmospheric Administration. May 22, 2011. Archived from the original on May 25, 2011. Retrieved May 22, 2011. Unknown parameter
|url-status=ignored (help) - ↑ Hart, John A.; Grams, Jeremy S. (May 24, 2011). Storm Prediction Center May 24, 2011 1630 UTC Day 1 Convective Outlook. Storm Prediction Center (Report). Norman, Oklahoma: National Oceanic and Atmospheric Administration. Archived from the original on October 28, 2011. Retrieved May 24, 2011. Unknown parameter
|url-status=ignored (help) - ↑ Mead, Corey M. (May 24, 2011). Particularly Dangerous Situation (PDS) Tornado Watch 356. Storm Prediction Center (Report). Norman, Oklahoma: National Oceanic and Atmospheric Administration. Archived from the original on September 3, 2014. Retrieved May 24, 2011. Unknown parameter
|url-status=ignored (help) - ↑ 6.0 6.1 "Storm Damage Assessment Toolkit". National Oceanic and Atmospheric Administration. Retrieved 2025-01-11.
- ↑ 7.0 7.1 7.2 "The Washington-Goldsby Tornado of May 24, 2011". NWS Norman, OK. NOAA. Archived from the original on February 11, 2017. Retrieved August 31, 2014. Unknown parameter
|url-status=ignored (help) - ↑ Jim LaDue; Tim Marshall; Kevin Scharfenberg (2012). "Discriminating EF4 and EF5 Tornado Damage". National Weather Service Office in Norman, Oklahoma. National Oceanic and Atmospheric Administration. Archived from the original (PDF) on January 9, 2016. Retrieved June 26, 2013. Unknown parameter
|name-list-style=ignored (help); Unknown parameter|url-status=ignored (help) - ↑ Yuko Murayama; Dimiter Velev; Plamena Zlateva (October 2019). Information Technology in Disaster Risk Reduction. Springer. ISBN 9783030321697. Archived from the original on 5 December 2022. Retrieved 5 December 2022. Unknown parameter
|url-status=ignored (help) Search this book on
- ↑ Cannon, Jane; Kimball, Michael (May 25, 2011). "Goldsby sustains damage but no injuries are reported". The Daily Oklahoman. Oklahoma City, Oklahoma. p. 6.
- ↑ "Multiple twisters cause injuries". The Daily Oklahoman. May 25, 2011. p. 4. Retrieved January 11, 2025.
