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{{Infobox weather event/EF
|multiple image={{multiple image | border = infobox | perrow = 1/2 | total_width = 250 | image1 = 2030 Moore tornado.png | image2 = May11MooreRadarLoop.gif|frameless}}
|image caption='''Top:''' The tornado as it approached the Orr Family Farm in western Moore.<br />'''Bottom:''' Radar loop of the tornado as it went through Moore.
|formed=May 11, 2030, 1:21 p.m. CDT (UTC-5:00)
|dissipated=May 11, 2030, 2:13 p.m. CDT (UTC-5:00)
|duration=46 minutes
|pathlength=15.1
|highest winds=205
|fatalities=35+
|injuries=315+
|damage-prefix=~
|damage=2100000000
|moneyyear=2030
|affected=Cleveland and Oklahoma Counties in Oklahoma, mainly the city of Moore
|tornado outbreak=[[Tornado outbreak of May 11-12, 2030]]
|tornado year=[[Tornadoes of 2030]]
}}
The '''2030 Moore tornado''' was a catastrophic and violent [[Enhanced Fujita scale|EF5 tornado]] that struck the city of [[Wikipedia:Moore, Oklahoma|Moore, Oklahoma]] on May 11, 2030. As part of a larger tornado outbreak affecting the Southern Plains, this tornado caused widespread devastation across Cleveland and Oklahoma counties, leaving a trail of destruction reminiscent of the deadly tornadoes that struck the region in 1999 and 2013. The tornado reached a peak intensity of EF5 on the Enhanced Fujita scale, with estimated winds of 205 mph (330 km/h), and carved a destructive path through densely populated areas, making it one of the most intense tornadoes to impact the United States in recent history.
The '''2030 Moore tornado''' was a catastrophic and violent [[Enhanced Fujita scale|EF5 tornado]] that struck the city of [[Wikipedia:Moore, Oklahoma|Moore, Oklahoma]] on May 11, 2030. As part of a larger tornado outbreak affecting the Southern Plains, this tornado caused widespread devastation across Cleveland and Oklahoma counties, leaving a trail of destruction reminiscent of the deadly tornadoes that struck the region in 1999 and 2013. The tornado reached a peak intensity of EF5 on the Enhanced Fujita scale, with estimated winds of 205 mph (330 km/h), and carved a destructive path through densely populated areas, making it one of the most intense tornadoes to impact the United States in recent history.


This was the third EF5 tornado to strike the city of Moore, following the devastating events of May 3, 1999, and May 20, 2013. It also marked the third EF5 tornado to occur in the United States since 2013, breaking a nearly two-decade lull in top-rated tornadoes. Despite the widespread damage throughout the city, the National Weather Service assigned the EF5 rating based on a single damage indicator: the complete destruction of a well-constructed restaurant in southern Moore. The rest of the tornado’s damage, while extreme, did not meet the threshold on its own for EF5 intensity.
This was the third EF5 tornado to strike the city of Moore, following the devastating events of May 3, 1999, and May 20, 2013. It also marked the third EF5 tornado to occur in the United States since 2013, breaking a nearly two-decade lull in top-rated tornadoes. Despite the widespread damage throughout the city, the National Weather Service assigned the EF5 rating based on a single damage indicator: the complete destruction of a well-constructed restaurant in southern Moore. The rest of the tornado’s damage, while extreme and consistent with EF4 intensity, did not meet the required damage indicators for an EF5 rating. However, the destruction of the restaurant, which had been bolted to its foundation and engineered to high standards, supported winds well over 200 mph.


== Meteorological synopsis ==
== Meteorological synopsis ==
[[File:May112030SPCOutlook.png|thumb|left|1630 UTC Day 1 outlook on May 11.]]
[[File:May112030SPCOutlook.png|thumb|left|1630 UTC Day 1 outlook on May 11.]]
On May 11, 2030, a potent combination of thermodynamic instability and strong wind shear set the stage for a significant tornado outbreak across the Southern Plains. In central Oklahoma, a surface low along a sharpening dryline intersected with a northward-lifting warm front, producing a volatile triple point environment. Surface temperatures reached 86 °F with dewpoints in the lower 70s °F, and CAPE values surged past 4400 J/kg. Steep lapse rates of 8.7 C/km in the 0-3 km layer and 7.4 C/km in the 3-6 km layer, along with SRH values nearing 460 m^2/s^2, indicated an atmosphere primed for tornadic supercells.
On May 11, 2030, an intense upper-level trough began to eject into the central United States, interacting with rich low-level moisture from the Gulf of Mexico and a strengthening surface low across the Texas Panhandle. A sharpening dryline extended into western Oklahoma, while a warm front lifted northward through central Oklahoma. This set the stage for a volatile triple point scenario across the Oklahoma City metro.


The Storm Prediction Center issued a Moderate Risk across Oklahoma, with a focused tornado threat zone near Moore and Oklahoma City. A Particularly Dangerous Situation (PDS) tornado watch was issued mid-afternoon. The environment supported intense, cyclic supercell thunderstorms capable of producing long-track tornadoes. As the afternoon progressed, multiple discrete supercells developed, with one tracking through Moore and producing the EF5 tornado that would go on to cause catastrophic damage and fatalities.
Thermodynamic conditions were highly supportive of violent tornadoes. Temperatures reached 86 °F with dewpoints near 73 °F, and mixed-layer CAPE values soared to over 4450 J/kg. Lapse rates were steep, measured at 8.7 C/km in the 0–3 km layer and 7.4 C/km in the 3–6 km layer, supporting strong updraft acceleration. Shear was equally concerning, with 0–1 km storm-relative helicity reaching 457 m²/s² and effective bulk shear in excess of 45 knots. Precipitable water (PWAT) values, although somewhat modest at 0.4 inches, were sufficient to support supercellular convection with strong inflow.
 
The Storm Prediction Center issued a Moderate Risk for severe weather across Oklahoma, with central Oklahoma placed under a Particularly Dangerous Situation (PDS) Tornado Watch during the early afternoon hours. The wording of the SPC discussion highlighted the risk of violent, long-track tornadoes. As the afternoon progressed, multiple discrete supercells formed along the dryline and quickly began producing tornadoes, culminating in the development of the deadly Moore EF5 tornado.


== Tornado ==
== Tornado ==


The 2030 Moore tornado touched down at approximately 1:21 p.m. CDT on May 11 near Newcastle, Oklahoma, rapidly intensifying as it moved northeast into the urban core of Moore. It followed a devastatingly similar path to previous tornadoes from 1999 and 2013, tracking for 15.1 miles and reaching maximum estimated winds of 205 mph (330 km/h). The tornado was on the ground for 46 minutes and maintained EF5 intensity across much of its path through central Moore.
The 2030 Moore tornado first touched down at 1:21 p.m. CDT near the rural outskirts of Newcastle, Oklahoma. Within minutes, the tornado underwent rapid intensification as it moved northeast, crossing into the city of Moore. Radar imagery showed a strong and rapidly intensifying mesocyclone, along with a pronounced debris ball. The tornado began widening significantly as it approached the western edge of Moore, ultimately reaching a peak width of approximately 1 mile.


Radar signatures showed a classic hook echo and a strong debris ball as the storm passed over the Orr Family Farm. The tornado widened to several hundred yards as it entered densely populated neighborhoods, destroying homes, schools, and medical facilities. Vehicles were thrown long distances, and entire subdivisions were leveled. The tornado dissipated around 2:13 p.m. CDT east of Lake Stanley Draper.
The tornado’s path closely mirrored those of the 1999 and 2013 Moore tornadoes, further compounding the emotional toll on residents. As it passed through residential neighborhoods and commercial corridors, entire structures were leveled, and several homes were swept completely clean from their foundations. The most intense damage occurred in the southern part of the city, where a well-built and anchor-bolted restaurant was completely obliterated. Vehicles were thrown and mangled, some tossed over a quarter-mile. The tornado maintained peak intensity through central Moore before gradually weakening and dissipating around 2:13 p.m. west of Lake Stanley Draper.


Despite the immense structural devastation across Moore, the National Weather Service based its EF5 rating on a single, highly specific damage indicator: the obliteration of a well-built, anchor-bolted restaurant structure in southern Moore. The destruction of this facility, which had been engineered to withstand high winds, supported wind estimates at or above the 200 mph threshold for EF5 classification.
Despite widespread destruction, EF5 classification was supported by only one structure: the aforementioned restaurant. The National Weather Service determined that its complete removal, coupled with the structural integrity and anchoring, justified a 205 mph wind estimate. Other damage indicators in the tornado's path, while extremely severe, were insufficient on their own for EF5 status and were rated high-end EF4.


== Impact ==
== Impact ==
[[File:Moore2030Damage.jpg|thumb|right|EF5 damage to a well-built restaurant in Moore.]]
[[File:Moore2030Damage.jpg|thumb|right|EF5 damage to a well-built restaurant in Moore.]]
Damage in Moore was extreme, with thousands of structures damaged or destroyed. Entire neighborhoods were reduced to bare foundations, and some homes were swept completely clean, indicative of EF5 damage. However, most structures were rated EF4 due to being lower-quality structures. The Orr Family Farm and nearby areas sustained catastrophic losses. A restaurant in southern Moore sustained EF5 damage, being the only structure to receive that rating. Two schools were either flattened or suffered major structural damage. Power lines, gas infrastructure, and roads were severely affected, complicating rescue and recovery efforts.
The tornado's impact on Moore was nothing short of devastating. Over 2,000 homes and businesses were damaged or destroyed across a swath of residential neighborhoods, shopping centers, schools, and critical infrastructure. Streets were rendered impassable due to massive debris fields. Entire subdivisions were reduced to rubble, and widespread power outages blanketed much of Cleveland and Oklahoma counties. Communications systems were temporarily knocked offline in some areas.


At least 35 people were confirmed killed, and over 315 others were injured. Emergency personnel from across the state converged on Moore for rescue operations, and multiple hospitals reported being at full capacity. The tornado caused an estimated $2.1 billion in damage, making it one of the costliest tornadoes in U.S. history. Thousands were left homeless, and debris removal efforts stretched into the following weeks.
The tornado claimed at least 35 lives and injured more than 315 people. Several victims were killed inside homes that lacked basements or safe rooms, while others were caught in vehicles or businesses. Hospitals in Moore and Oklahoma City were overwhelmed with trauma cases, prompting emergency medical transports from surrounding counties. The financial toll was enormous, with damage estimates approaching $2.1 billion (2030 USD), ranking it among the most expensive tornadoes in U.S. history.


Much of the worst damage occurred in well-developed residential zones, where even homes built to post-2013 enhanced standards were destroyed. Cars and trucks were thrown hundreds of yards and mangled beyond recognition. Numerous trees were debarked, and many survivors described the sound of the storm as louder than a freight train. The rapid arrival and intense violence of the tornado gave residents little time to react, despite timely warnings.
In addition to the destruction of homes, two schools were either destroyed or sustained heavy damage. The Orr Family Farm, a well-known local landmark, was flattened along with adjacent equestrian facilities. Emergency responders, aided by volunteers and search dogs, worked through the night in dangerous conditions to search for survivors. Many residents credited timely warnings from local broadcasters and weather radios for saving lives, though the intensity and speed of the tornado still left little time to act.


== Aftermath ==
== Aftermath ==
In the aftermath of the tornado, local, state, and federal authorities declared a state of emergency. The Oklahoma National Guard and FEMA were deployed to assist with recovery. Temporary shelters were opened in unaffected parts of the city, and schools in surrounding communities were closed to facilitate housing and aid operations. Major utility disruptions persisted for days as crews worked to restore power and services.


The event prompted renewed discussions about the construction of storm shelters and safe rooms in residential homes and public buildings. Although Moore had adopted improved building codes after the 2013 tornado, the EF5 winds exceeded even enhanced structural designs in some areas. The tragedy reignited calls for nationwide reforms in tornado-resilient building practices, especially in high-risk regions.
Following the disaster, a federal emergency was declared, and extensive resources were mobilized. The Oklahoma National Guard established perimeter security and assisted with search and rescue, while FEMA coordinated the deployment of urban search teams, temporary housing units, and debris clearance. More than 30 shelters were opened across the metro, many housed in church gyms and school auditoriums.
 
The tornado reignited national discussions about storm safety and construction standards. Moore, having already adopted stricter building codes after 2013, now faced questions about whether even those improved standards were sufficient. Engineers began studying the destroyed restaurant and other structural failures to inform future building designs in tornado-prone areas.


Volunteers from across the country came to assist in clean-up and aid efforts. Relief funds were established by state and national charities, while local organizations provided food, supplies, and emotional support. The city of Moore began long-term rebuilding plans shortly after, committing to stronger safety measures and reinforcing public infrastructure to better withstand future storms.
Volunteers poured in from around the country. Charitable organizations coordinated donations, food drives, and trauma counseling. Within weeks, city leaders began to outline long-term rebuilding plans, which emphasized storm shelter installations, enhanced community alert systems, and infrastructure reinforcement. The tragedy also prompted emergency management offices nationwide to revisit public outreach strategies for severe weather preparedness.


== See also ==
== See also ==
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{{main|Tornado outbreak of May 11-12, 2030}}
{{main|Tornado outbreak of May 11-12, 2030}}


The 2030 Moore tornado was the most destructive tornado in a two-day outbreak that produced 19 confirmed tornadoes across Oklahoma, Kansas, and Missouri. Alongside the Moore tornado, the outbreak included the [[2030 El Reno tornado|2030 El Reno EF4 tornado]] and several EF2–EF3 events. The moderate-risk forecast verified with multiple cyclic supercells and high-end thermodynamic profiles contributing to violent tornado development across the Southern Plains.
The 2030 Moore tornado was the most destructive tornado in a two-day outbreak that produced 19 confirmed tornadoes across Oklahoma, Kansas, and Missouri. Alongside the Moore tornado, the outbreak included the [[2030 El Reno tornado|2030 El Reno EF4 tornado]] and several EF2–EF3 events. The moderate-risk forecast verified with multiple cyclic supercells and high-end thermodynamic profiles contributing to violent tornado development across the Southern Plains. The outbreak reaffirmed central Oklahoma’s unfortunate status as one of the most tornado-prone regions in the world.

Revision as of 22:32, 29 April 2025

The 2030 Moore tornado was a catastrophic and violent EF5 tornado that struck the city of Moore, Oklahoma on May 11, 2030. As part of a larger tornado outbreak affecting the Southern Plains, this tornado caused widespread devastation across Cleveland and Oklahoma counties, leaving a trail of destruction reminiscent of the deadly tornadoes that struck the region in 1999 and 2013. The tornado reached a peak intensity of EF5 on the Enhanced Fujita scale, with estimated winds of 205 mph (330 km/h), and carved a destructive path through densely populated areas, making it one of the most intense tornadoes to impact the United States in recent history.

This was the third EF5 tornado to strike the city of Moore, following the devastating events of May 3, 1999, and May 20, 2013. It also marked the third EF5 tornado to occur in the United States since 2013, breaking a nearly two-decade lull in top-rated tornadoes. Despite the widespread damage throughout the city, the National Weather Service assigned the EF5 rating based on a single damage indicator: the complete destruction of a well-constructed restaurant in southern Moore. The rest of the tornado’s damage, while extreme and consistent with EF4 intensity, did not meet the required damage indicators for an EF5 rating. However, the destruction of the restaurant, which had been bolted to its foundation and engineered to high standards, supported winds well over 200 mph.

Meteorological synopsis

1630 UTC Day 1 outlook on May 11.

On May 11, 2030, an intense upper-level trough began to eject into the central United States, interacting with rich low-level moisture from the Gulf of Mexico and a strengthening surface low across the Texas Panhandle. A sharpening dryline extended into western Oklahoma, while a warm front lifted northward through central Oklahoma. This set the stage for a volatile triple point scenario across the Oklahoma City metro.

Thermodynamic conditions were highly supportive of violent tornadoes. Temperatures reached 86 °F with dewpoints near 73 °F, and mixed-layer CAPE values soared to over 4450 J/kg. Lapse rates were steep, measured at 8.7 C/km in the 0–3 km layer and 7.4 C/km in the 3–6 km layer, supporting strong updraft acceleration. Shear was equally concerning, with 0–1 km storm-relative helicity reaching 457 m²/s² and effective bulk shear in excess of 45 knots. Precipitable water (PWAT) values, although somewhat modest at 0.4 inches, were sufficient to support supercellular convection with strong inflow.

The Storm Prediction Center issued a Moderate Risk for severe weather across Oklahoma, with central Oklahoma placed under a Particularly Dangerous Situation (PDS) Tornado Watch during the early afternoon hours. The wording of the SPC discussion highlighted the risk of violent, long-track tornadoes. As the afternoon progressed, multiple discrete supercells formed along the dryline and quickly began producing tornadoes, culminating in the development of the deadly Moore EF5 tornado.

Tornado

The 2030 Moore tornado first touched down at 1:21 p.m. CDT near the rural outskirts of Newcastle, Oklahoma. Within minutes, the tornado underwent rapid intensification as it moved northeast, crossing into the city of Moore. Radar imagery showed a strong and rapidly intensifying mesocyclone, along with a pronounced debris ball. The tornado began widening significantly as it approached the western edge of Moore, ultimately reaching a peak width of approximately 1 mile.

The tornado’s path closely mirrored those of the 1999 and 2013 Moore tornadoes, further compounding the emotional toll on residents. As it passed through residential neighborhoods and commercial corridors, entire structures were leveled, and several homes were swept completely clean from their foundations. The most intense damage occurred in the southern part of the city, where a well-built and anchor-bolted restaurant was completely obliterated. Vehicles were thrown and mangled, some tossed over a quarter-mile. The tornado maintained peak intensity through central Moore before gradually weakening and dissipating around 2:13 p.m. west of Lake Stanley Draper.

Despite widespread destruction, EF5 classification was supported by only one structure: the aforementioned restaurant. The National Weather Service determined that its complete removal, coupled with the structural integrity and anchoring, justified a 205 mph wind estimate. Other damage indicators in the tornado's path, while extremely severe, were insufficient on their own for EF5 status and were rated high-end EF4.

Impact

EF5 damage to a well-built restaurant in Moore.

The tornado's impact on Moore was nothing short of devastating. Over 2,000 homes and businesses were damaged or destroyed across a swath of residential neighborhoods, shopping centers, schools, and critical infrastructure. Streets were rendered impassable due to massive debris fields. Entire subdivisions were reduced to rubble, and widespread power outages blanketed much of Cleveland and Oklahoma counties. Communications systems were temporarily knocked offline in some areas.

The tornado claimed at least 35 lives and injured more than 315 people. Several victims were killed inside homes that lacked basements or safe rooms, while others were caught in vehicles or businesses. Hospitals in Moore and Oklahoma City were overwhelmed with trauma cases, prompting emergency medical transports from surrounding counties. The financial toll was enormous, with damage estimates approaching $2.1 billion (2030 USD), ranking it among the most expensive tornadoes in U.S. history.

In addition to the destruction of homes, two schools were either destroyed or sustained heavy damage. The Orr Family Farm, a well-known local landmark, was flattened along with adjacent equestrian facilities. Emergency responders, aided by volunteers and search dogs, worked through the night in dangerous conditions to search for survivors. Many residents credited timely warnings from local broadcasters and weather radios for saving lives, though the intensity and speed of the tornado still left little time to act.

Aftermath

Following the disaster, a federal emergency was declared, and extensive resources were mobilized. The Oklahoma National Guard established perimeter security and assisted with search and rescue, while FEMA coordinated the deployment of urban search teams, temporary housing units, and debris clearance. More than 30 shelters were opened across the metro, many housed in church gyms and school auditoriums.

The tornado reignited national discussions about storm safety and construction standards. Moore, having already adopted stricter building codes after 2013, now faced questions about whether even those improved standards were sufficient. Engineers began studying the destroyed restaurant and other structural failures to inform future building designs in tornado-prone areas.

Volunteers poured in from around the country. Charitable organizations coordinated donations, food drives, and trauma counseling. Within weeks, city leaders began to outline long-term rebuilding plans, which emphasized storm shelter installations, enhanced community alert systems, and infrastructure reinforcement. The tragedy also prompted emergency management offices nationwide to revisit public outreach strategies for severe weather preparedness.

See also

Tornado outbreak of May 11-12, 2030

2030 El Reno tornado

2013 Moore tornado

1999 Bridge Creek–Moore tornado

2023 Rolling Fork tornado

Part of

The 2030 Moore tornado was the most destructive tornado in a two-day outbreak that produced 19 confirmed tornadoes across Oklahoma, Kansas, and Missouri. Alongside the Moore tornado, the outbreak included the 2030 El Reno EF4 tornado and several EF2–EF3 events. The moderate-risk forecast verified with multiple cyclic supercells and high-end thermodynamic profiles contributing to violent tornado development across the Southern Plains. The outbreak reaffirmed central Oklahoma’s unfortunate status as one of the most tornado-prone regions in the world.