The 1999 Bridge Creek–Moore tornado (locally referred to as the May 3rd tornado) was an extremely powerful F5 tornado in which the highest wind speeds ever measured globally were recorded at 301 ± 20 miles per hour (484 ± 32 km/h) by a Doppler on Wheels (DOW) radar. The tornado devastated southern portions of Oklahoma City, Oklahoma, along with surrounding suburbs and towns during the early evening of Monday, May 3, 1999. The tornado covered 38 miles (61 km) during its 85-minute existence, destroying thousands of homes, killing 36 people (plus an additional five indirectly), and leaving US$1 billion (1999 USD) in damage, ranking it as the fifth-costliest on record, not accounting for inflation.
The tornado first touched down at 6:23 p.m. Central Daylight Time (CDT) in Grady County, Oklahoma, roughly two miles (3.2 km) south-southwest of Amber, Oklahoma. It quickly intensified into a violent F4, and gradually reached F5 status after traveling 6.5 miles (10.5 km), at which time it struck the town of Bridge Creek. It fluctuated in strength, ranging from F2 to F5 status before it crossed into Cleveland County where it reached F5 intensity for a third time shortly before entering the city of Moore. By 7:30 p.m., the tornado crossed into Oklahoma County and battered southeastern Oklahoma City, Del City, and Midwest City before dissipating around 7:48 p.m. just outside Midwest City. A total of 8,132 homes, 1,041 apartments, 260 businesses, 11 public buildings, and 7 churches were damaged or destroyed.
Large-scale search and rescue operations immediately took place in the affected areas. A major disaster declaration was signed by President Bill Clinton the following day (May 4) allowing the state to receive federal aid. In the following months, disaster aid amounted to $67.8 million. Reconstruction projects in subsequent years led to a safer, tornado-ready community. In May 2013, similar areas adjacent to the 1999 storm's track were again devastated by an EF5 tornado, resulting in 24 fatalities and extreme damage in the South Oklahoma City/Moore area.
|1999 Bridge Creek–Moore tornado|
The tornado near peak intensity
|Formed||May 3, 1999, 6:23 p.m. CDT (UTC−05:00)|
|Duration||1 hour, 25 minutes|
|Dissipated||May 3, 1999, 7:48 p.m. CDT (UTC−05:00)|
|Max rating1||F5 tornado|
|Damage||$1 billion (1999 USD)|
$1.5 billion (2019 USD)
|Fatalities||36 fatalities (+5 indirect),|
|Areas affected||Grady, McClain, Cleveland and Oklahoma counties in Oklahoma; with the worst impacts occurring in the towns/cities of Bridge Creek, Moore, Oklahoma City, Del City, and Midwest City|
|1Most severe tornado damage; see Fujita scale Part of the 1999 Oklahoma tornado outbreak|
The Bridge Creek–Moore tornado was part of a much larger outbreak, which produced 71 tornadoes across five states throughout the Central Plains on May 3 alone, along with an additional 25 that touched down a day later in some of the areas affected by the previous day's activity (some of which were spawned supercells that developed on the evening of May 3), stretching eastward to the Mississippi River Valley. On the morning of May 3, in its Day 1 Convective Outlook for the United States, the Storm Prediction Center (SPC) issued a slight risk for severe weather, as a dry line that stretched from western Kansas into western Texas approached a warm, humid air-mass over the Central Plains; the conditions ahead of the dry line and a connecting trough positioned over northeastern Colorado appeared to favor the development of thunderstorms later that day that would contain large hail, damaging straight-line winds, and isolated tornadoes.
Forecasters at the SPC initially underestimated the atmospheric conditions that would support tornadic development that afternoon and evening; around 4:00 a.m. CDT, Doppler radar and wind profile data indicated a 90-knot (100 mph; 170 km/h) jet stream along the border of California and Nevada, with weather balloon soundings sent up the previous evening by National Weather Service offices in the western United States and numerical computer model data failing to detect the fast-moving air current as it moved ashore from the Pacific Ocean. In addition, the dry line was diffused, with surface winds behind and ahead of the boundary moving into the region from a southerly direction. SPC meteorologists began to recalculate model data during the morning to account for the stronger wind profiles caused by the jet streak; the data acknowledged that thunderstorms would occur within the Central Plains, but disagreed on the exact area of greatest severe weather risk.
By 7:00 a.m. Central Daylight Time, CAPE values began exceeding 4,000 J/kg, a level that climatologically favors the development of severe thunderstorms. Despite conflicting model data on the specified area where thunderstorms would develop, the newly available information that denoted a more favorable severe thunderstorm setup in that part of the state prompted the SPC to upgrade the forecasted threat of severe weather to a moderate risk for south-central Kansas, much of the western two-thirds of Oklahoma, and the northwestern and north-central portions Texas at 11:15 a.m. CDT that morning, which now indicated an elevated threat of strong tornadoes.
By the early afternoon hours, forecasters at both the SPC and the National Weather Service Weather Forecast Office in Norman, Oklahoma, realized that a major event was likely to take place based solely on observational data from radar and weather satellite imagery and balloon soundings, as the computer models remained uncooperative in helping meteorologists determine where the greatest threat of severe storms would occur.
Conditions became highly conducive for tornadic development by 1:00 p.m. CDT as wind shear intensified over the region (as confirmed by an unscheduled balloon sounding flight conducted by the NWS Norman office), creating a highly unstable atmosphere. The sounding balloon recorded winds blowing southwesterly at 20 mph (32 km/h) and 50 mph (80 km/h) respectively at the surface and at the 12,000-foot (3,700 m) level, southerly winds of 40 mph (64 km/h) and westerly winds of 20 mph (32 km/h) at 20,000 feet (6,100 m); it also indicated that a capping inversion over the region was weakening in southwestern Oklahoma and north Texas; with the warm air above the surface cooling down, this allowed warm air at the surface the chance to rise and potentially create thunderstorms. Although cirrus clouds − a bank of which had developed in west Texas and overspread portions of Oklahoma later in the morning − were present through much of the day, an area of clearing skies over western north Texas and southwestern Oklahoma early that afternoon allowed for the sun to heat up the moisture-laden region, creating significant atmospheric instability.
At 3:49 p.m. CDT, the Storm Prediction Center issued a high severe weather risk for much of central Oklahoma. Within 25 minutes of this, the National Weather Service office in Norman issued a severe thunderstorm warning for Comanche County by 4:15 p.m. CDT late that afternoon, as the first storm of the event rapidly intensified. A half-hour later, at 4:45 p.m. CDT, the Storm Prediction Center issued a tornado watch for western and central Oklahoma for the threat of tornadoes, hail up to 3 inches (7.6 cm) in diameter, and wind gusts to 80 mph (130 km/h).
The thunderstorm that eventually produced the F5 tornado formed around 3:30 p.m. CDT over Tillman County. Despite the lack of overall lift prevalent in the region, the storm formed out of a contrail-like horizontal area of convective clouds that developed during peak surface heating over southwestern Oklahoma, located well ahead of the dry line still positioned farther to the west, which provided enhanced lift and speed shear necessary to develop the supercell. Tracking northeast, the storm strengthened and entered Comanche County shortly after 4:00 p.m. CDT; there, hail up to 1.75 inches (4.4 cm) in diameter fell.
As the rotation in the supercell began to rapidly increase at the cloud base, a tornado warning was issued for the counties of Comanche, Caddo, and Grady at 4:50 p.m. CDT; one minute later, a small tornado roughly 25 yards (75 ft) in diameter − the first of 14 associated with supercell "A" (the National Weather Service Weather Forecast Office in Norman designated lettered names for the three tornado-producing supercells in the outbreak in storm surveys) − touched down seven miles (11 km) east-northeast of Medicine Park along U.S. Route 62. Five more tornadoes developed as the storm continued northeast; a sixth one, this being an F3, touched down a short time later and caused substantial damage in central Grady County, including some to the Chickasha Municipal Airport, where roofs were torn off of two hangars. At 6:23 p.m. CDT, a ninth tornado associated with supercell "A" touched down about 2 miles (3.2 km) south-southwest of Amber.
The tornado quickly intensified as it crossed Oklahoma State Highway 92, attaining F4 strength about 4 miles (6.4 km) east-northeast of Amber. Damage consistent with this rating was sustained over the following 6.5 miles (10.5 km) of the path before striking Bridge Creek. There, it attained the highest-possible rating on the Fujita Scale, F5. Damage in this area was extreme, as many homes were swept away completely, leaving only concrete slabs where the structures once stood. Damage surveyors noted that the remaining structural debris from some of the homes in this area was finely granulated into small fragments, and that trees and shrubs were completely debarked. A few of these homes were bolted to their foundations. Extensive ground scouring occurred, and vehicles were thrown hundreds of yards from where they originated, including a mangled pickup truck that was found wrapped around a telephone pole. It was in this area that a mobile Doppler weather radar recorded winds of 301 mph (484 km/h) within the tornado, the highest wind speed ever recorded on Earth. Since the record for maximum winds are reported from only non-tornadic events, however, the 253 mph (407 km/h) wind gust from Cyclone Olivia in 1996 retained the title. About 1 inch (25 mm) of asphalt was scoured off a road by the violent tornado. Approximately 200 mobile homes/houses were destroyed, and hundreds of other structures were damaged. The Ridgecrest Baptist Church in Bridge Creek was also destroyed in the process. About 12 people died in Bridge Creek, nine of whom were in mobile homes; all fatalities and the majority of injuries were concentrated in the Willow Lake and Southern Hills Additions and Bridge Creek Estates, consisting mostly of mobile homes. Over 39 people were injured in the area as well. Continuing northeastward, the tornado briefly weakened to F4 status before re-strengthening to F5 intensity as it neared the Grady-McClain County line, where a car was thrown roughly 0.25 mi (0.40 km) in the air, and a well-built home with anchor bolts was reduced to a bare slab. At this time, it had attained a width of one mile (1.6 km).
Around 6:57 p.m. CDT, the National Weather Service Forecast Office in Norman issued the first-ever tornado emergency for southern portions of the Oklahoma City metropolitan area, which was released as a standalone weather statement (instead of within a newly issued or a Special Weather Statement on an existing tornado warning, as became usual afterward). David Andra, a meteorologist at the NWS Norman office, said that he drafted the enhanced warning statement to "paint the picture that a rare and deadly tornado was imminent in the metro area."
Paralleling along Interstate 44, the tornado moved into McClain County, where it crossed the highway twice at F4 intensity, killing a woman as she was blown out from an underpass where she was attempting to seek shelter, after being dragged down the embankment by the intense channeling winds; her 11-year-old son − with whom the woman vacated their stalled car nearby − survived, staying held tight onto the steel girders of the overpass. A man who helped the mother and son up the overpass suffered severe injuries to his leg, which was partially sliced by a highway sign thrown by the winds. At 7:10 p.m. CDT, a satellite tornado touched down over an open field north of Newcastle; it was rated as an F0 due to lack of damage. 38 homes and two businesses were destroyed in McClain County, and 40 homes were flattened; some of these homes were leveled at F4 intensity, and 17 people were injured.
After crossing the Canadian River, the tornado entered Cleveland County and weakened to F2 intensity. By this time, it had entered the south side of Oklahoma City. Several minutes after entering the county, it re-attained F4 status, and then moved directly into the city of Moore, reaching F5 intensity for a third time. Some of the most severe damage took place in Cleveland County, mainly in Moore, where 11 people were killed and 293 others were injured. The tornado caused an estimated $450 million in damage across the county. The first area impacted in Moore was the Country Place Estates subdivision, where 50 homes were destroyed and one was swept cleanly from its foundation at F5 intensity. Several vehicles were picked up and tossed nearly 0.25 mi (0.40 km). According to local police, an airplane wing, believed to have been from an airport in Grady County, was found near Country Place Estates. Then, the powerful tornado struck the densely populated Eastlake Estates at F5 intensity, killing three people and reducing entire rows of homes to rubble. In one instance, four adjacent homes were completely destroyed, with only concrete slabs remaining, warranting an F5 rating at that location. Three other homes in this housing division also received F5 damage, with the remaining destruction rated high-end F4. Severe debarking of trees was noted in this area. At the Emerald Springs Apartments, three more people were killed and a two-story apartment building was mostly flattened.
As it entered Cleveland County, the National Weather Service and Storm Prediction Center activated emergency procedures, preparing to evacuate staff and others present at the facility in the event that the supercell should turn right, placing areas surrounding the Norman campus in the tornado's path (under NOAA protocol in situations posing a danger to personnel at local Weather Forecast Offices and related guidance centers, responsibility over the issuance of warnings and statements on the unfolding outbreak would have been transferred to the nearest NWS Forecast Office, based in Tulsa, while the SPC's forecasting responsibilities would be turned over to the 557th Weather Wing at Offutt Air Force Base). The supercell, however, continued on a northeastward track, sparing the Norman area.
Safety precautions were also enacted elsewhere in and near the storm's path; council members and citizens at Moore City Hall − where a council meeting was scheduled to be held that evening − sheltered in place in the building's first-floor restrooms, away from the multiple large-pane windows at its facade. In downtown Oklahoma City, spectators attending sporting events held that evening involving two of the city's minor league teams – a regular season baseball game between the Oklahoma RedHawks and Memphis Redbirds (which was suspended during the second inning) and Game 2 of the Ray Miron President's Cup series between the Oklahoma City Blazers and the Huntsville Channel Cats – were also evacuated to shelter in an underground storage area connected to the Southwestern Bell Bricktown Ballpark and Myriad Convention Center amid concerns that the storm would jog northward and place Oklahoma City itself in the tornado's path. Flights were grounded at Will Rogers World Airport as the northern edge of the supercell approached the area; the tornado turned right, away from southwestern parts of the city proper, shortly before airport officials began evacuating employees and visitors at the terminals. Traffic on Interstate 35 in south Oklahoma City and north Moore became backed up for several miles, as drivers evacuated from their vehicles to seek shelter under an overpass overlooking South Shields Boulevard.
Just outside the Eastlake Estates, an honors ceremony was being held at Westmoore High School at the time of the tornado. Adequate warning time allowed those at the school to seek shelter, however, and more than 400 adults and children attending the awards ceremony at the school's auditorium were moved to the main building, sheltering in reinforced hallways and bathrooms. Ultimately, Westmoore High sustained heavy damage and dozens of cars in the parking lot were tossed around, some of which were completely destroyed or thrown into nearby homes. No injuries took place at the school, though a horse was found dead between a couple of destroyed cars in this area. The tornado proceeded through additional densely populated areas of Moore shortly thereafter, where several large groups of homes were flattened in residential areas, with a mixture of high-end F4 and low-end F5 damage noted. Near Janeway Avenue, four people were killed in an area where multiple homes were completely destroyed. A woman, who took shelter with her husband and two children, was also killed when she was blown out from under the Shields overpass on Interstate 35. The tornado weakened somewhat as it moved through the Highland Park neighborhood of Moore, but still caused widespread F3 and F4 damage.
The tornado then entered Oklahoma County and struck the southeast fringes of Oklahoma City, where it re-intensified to high-end F4 strength and two people were killed as a trucking company was completely destroyed. Shortly before it tracked into the county, patrons and employees at Crossroads Mall were evacuated to storage areas in the basement of the building. Numerous industrial buildings were leveled in this area of the city. A freight car, weighing 36,000 lb (16,000 kg) was thrown 0.75 mi (1.21 km). The car bounced as it traveled, remaining airborne for 50 to 100 yd (46 to 91 m) at a time. Multiple homes were also completely destroyed in southeast Oklahoma City, and one woman was killed in that area. Crossing Southeast 44th Street into Del City, the tornado moved through the highly populated Del Aire housing addition, killing six people and damaging or destroying hundreds of homes, with many sustaining F3 to F4 damage. Seven people were killed as a direct result of the tornado in Del City, and hundreds of homes were damaged or destroyed.
The tornado then crossed Sooner Road, damaged an entry gate and several buildings at Tinker Air Force Base, then crossed 29th Street into Midwest City, destroying one building at the Boeing Complex and damaging two others. Widespread F3/F4 damage continued as the tornado moved across Interstate 40, affecting a large business district. Approximately 800 vehicles at Hudiburg Auto Group were damaged, located just south of Interstate 40. Hundreds of vehicles at the dealership were moved from their original location on the lot, and dozens of vehicles (including 30 awaiting tune-ups or repairs at Morris' Auto Machine and Supply, and an unoccupied Mid-Del School District bus) were picked up and tossed northward across the interstate into several motels, a distance of approximately two-tenths of a mile. Numerous motels and other businesses including Hampton Inn, Comfort Inn, Inn Suites, Clarion Inn, Cracker Barrel, and portions of Rose State College, were destroyed. While some of the damage through this area was rated high-end F4, low-end F5 was considered. The tornado then continued into another residential area located between Southeast 15th and Reno Avenue, where three fatalities occurred. Damage consistent with high-end F4 wind speeds was inflicted to four homes in this area. Two of these homes were located between Southeast 11th and 12th Streets, near Buena Vista, and the other two homes were located on Will Rogers Road, just south of Southeast 15th. Damage then diminished rapidly to F0/F1 strength as the tornado crossed Reno Avenue, before dissipating three blocks north of Reno, between Sooner Road and Air Depot Boulevard. Throughout Oklahoma County, 12 people were killed and 234 others were injured while losses amounted to $450 million.
Thirty-six people were killed as a direct result of the storm and five more died of indirect causes in the hours following it; most of the indirect deaths were due to heart attacks or injuries suffered while trying to seek shelter. One survivor was uninjured but died from a self-inflicted gunshot wound. According to the Oklahoma Department of Health, an estimated 583 people were injured by the tornado, accounting for those who did not go to the hospital or were unaccounted for. A total of 8,132 homes, 1,041 apartments, 260 businesses, 11 public buildings, and 7 churches were damaged or destroyed. Estimated damage costs totaled $1.2 billion, making it the first recorded tornado to exceed $1 billion. The Bridge Creek−Moore tornado produced an estimated 220 cubic yards (170 m3) of debris from the buildings that were destroyed.
This was the deadliest tornado recorded in Oklahoma since an F5 tornado killed 107 people in Woodward on April 9, 1947. It was also the deadliest tornado ever recorded in the Oklahoma City metropolitan area; the previous record was held by an F4 tornado that affected southwestern portions of the city on June 12, 1942, killing 31 people and causing $500,000 in damage ($11.2 million in (2019 USD) when adjusted for inflation). It was the costliest tornado in US history until an EF4 tornado hit Tuscaloosa and northern portions of Birmingham, Alabama on April 27, 2011, causing an estimated $2.45 billion in damage (as of 2015, the Bridge Creek–Moore tornado is the fourth-costliest tornado, having been surpassed by the EF5 tornadoes that hit Joplin on May 22, 2011, and areas of Moore near the 1999 storm track on May 20, 2013). National Weather Service researchers estimated that the death toll from the storm would likely have exceeded 600 had it not been for the advanced warning through local television and radio stations and exercising proper safety precautions.
Following the outbreak of deadly and destructive tornadoes, President Bill Clinton signed a major disaster declaration for eleven Oklahoma counties on May 4. In a press statement by the Federal Emergency Management Agency (FEMA), then-director James Lee Witt stated that "The President is deeply concerned about the tragic loss of life and destruction caused by these devastating storms." The American Red Cross opened ten shelters overnight across central Oklahoma, housing 1,600 people immediately following the disaster. By May 5, this number had lowered to 500. Throughout May 5, several post-disaster teams from FEMA were deployed to the region, including emergency response and preliminary damage assessment units. The United States Department of Defense deployed the 249th Engineering Battalion and placed the U.S. Army Corps of Engineers on standby for assistance. Medical and mortuary teams were also sent by the Department of Health and Human Services. By May 6, donation centers and phone banks were being established to create funds for victims of the tornadoes.
Continuing search and rescue efforts for thirteen people who were listed as missing through May 7 were assisted by urban search and rescue dogs from across the country. Nearly 1,000 members of the Oklahoma National Guard were deployed throughout the affected region. The American Red Cross had set up ten mobile feeding stations by this time and stated that 30 more were en route. On May 8, a disaster recovery center was opened in Moore for individuals recovering from the tornadoes. According to the Army Corps of Engineers, roughly 500,000 cubic yards (382,277 cubic meters) of debris was left behind and would likely take weeks to clear. Within the first few days of the disaster declaration, relief funds began being sent to families who requested aid. By May 9, roughly $180,000 had been approved by FEMA for disaster housing assistance.
Debris removal finally began on May 12 as seven cleanup teams were sent to the region, more were expected to join over the following days. That day, FEMA also declared that seven counties − Canadian, Craig, Grady, Lincoln, Logan, Noble and Oklahoma − were eligible for federal financial assistance. By May 13, roughly $1.6 million in disaster funds had been approved for housing and businesses loans. This quickly rose to more than $5.9 million over the following five days. By May 21, more than 3,000 volunteers from across the country traveled to Oklahoma to help residents recover; 1,000 of these volunteers were sent to Bridge Creek to clean up debris, cut trees, sort donations and cook meals. With a $452,199 grant from FEMA, a 60-day outreach program for victims suffering tornado-related stress was set up to help them cope with trauma.
Applications for federal aid continued through June, with state approvals reaching $54 million on June 3. By this date, the Army Corps of Engineers reported that 964,170 cubic yards (737,160 cubic meters), roughly 58%, of the 1.65 million cubic yards (1.26 million cubic meters) of debris had been removed. Assistance for farmers and ranchers who suffered severe losses from the tornadoes was also available by June 3. After more than a month of being open, emergency shelters were set to be closed on June 18. On June 21, an educational road show made by FEMA visited the hardest hit areas in Oklahoma to urge residents to build storm cellars. According to FEMA, more than 9,500 residents applied for federal aid during the allocated period in the wake of the tornadoes. Most of the applicants lived in Oklahoma and Cleveland counties, 3,800 and 3,757 persons respectively. In all, disaster recovery aid for the tornadoes amounted to roughly $67.8 million by the end of July 2.
Over the following four years, a $12 million project to construct storm shelters for residents across the Oklahoma City metropolitan area was enacted. The goal was to create a safer community in a tornado-prone region. By May 2003, a total of 6,016 safe rooms were constructed. On May 9, 2003, the new initiative was put to the test as a tornado outbreak in the region spawned an F4 tornado, which took a path similar to that of the Bridge Creek–Moore tornado. Due to the higher standards for public safety, no one was killed by the 2003 tornado, a substantial improvement in just four years. On May 20, 2013, an EF5 tornado impacted some of the same areas affected by the 1999 storm, tracking through the heart of Moore. Throughout the city, 24 people were killed (along with one additional person who died as an indirect result of the tornado) and more than 230 were injured.
From a meteorological and safety standpoint, the tornado also brought the use of highway overpasses as shelters into question. Prior to the events on May 3, 1999, videos of people taking shelter in overpasses during tornadoes in the past (most notably one filmed near Wichita, Kansas, during the April 26, 1991 tornado outbreak involving a television news crew from Wichita NBC affiliate KSNW and other bystanders) gave the public misunderstanding that overpasses provided shelter from tornadoes. For nearly 20 years, meteorologists had questioned the safety of these structures; they lacked incidents involving loss of life, however. During the May 3 outbreak, three overpasses were directly struck by tornadoes, with a fatality taking place at each one. Two of these were from the F5 Bridge Creek–Moore tornado while the third was from a small F2, which struck a rural area in Payne County, north-northeast of Oklahoma City. According to a study by the National Oceanic and Atmospheric Administration, seeking shelter in an overpass "is to become a stationary target for flying debris."
Preliminary damage surveys conducted by a group of structural engineers from Texas Tech University determined that many of the frame homes that were destroyed by the Bridge Creek−Moore tornado were constructed below minimal residential building code standards, discovering some structural deficiencies that violated codes, which were considered to be inadequate for regions prone to tornadic activity (under federal building code standards, frame homes that were properly strapped and bolted would have withstood winds between 152 and 157 miles per hour (245 and 253 km/h), equivalent to an F2 tornado). The team, led by meteorological researcher Charles Doswell and storm damage engineer/meteorologist Tim Marshall, determined that nails attached to a plywood roof deck in one damaged home were not properly anchored to the rafters; several homes in rural areas that were swept nearly 300 feet (91 m) from their original location did not have anchor bolts that secured the frame to their foundations, as was the case at Country Place Estates, where the homes − which left a trail of debris strewn 3,000 feet (910 m) away from their location − were attached to the concrete foundations by tapered cut nails that extended only a half-inch to the bases; many homes that were left at least partially standing also had their garage doors (mainly those made from aluminum material) collapse inward, allowing the tornado's destructive winds to enter the houses.
Marshall discovered other building and vehicle remains that became debris missiles, including a twisted 36-inch (0.91 m) steel beam, a steel leg broken off of a lawn chair that was impaled into a 5-by-5-inch (13 cm × 13 cm) post by the violent winds and a six-foot (180 cm) section of a sewer pipe that was blown into the interior hallway of one house through the front door. The team's findings also revealed that several homes were obliterated before they experienced the full impact of the vortex's peak wind velocities, with some disintegrating as the external winds surrounding the parent tornado reached speeds of F2 intensity. Three months later, as homes were being built in the damage path, Marshall found their construction to be scarcely superior to that of the homes destroyed in the May 3 storm.
The Federal Emergency Management Agency (FEMA) corroborated with Doswell and Marshall's findings in its Building Performance Assessment Team Report on the May 3 outbreak, noting that much of the structural damage resulted from strong winds generated by the tornado and associated windborne debris that often "produced forces on buildings not designed to withstand such forces" and in some cases, were due to improper construction techniques and "poor selection" of materials used in their construction. The report acknowledged that federal construction code requirements needed to be revised above the then-current minimum standards to allow newer buildings to better withstand higher wind speeds consistent with tornadoes of lesser intensity than the one that devastated Bridge Creek and Moore, thereby lessening the degree of damage, fatalities and injuries that are probable in buildings of typically less reinforced construction.
Wichita Falls, Tx. (1979)
| Costliest U.S. tornadoes on Record
May 3, 1999
Tuscaloosa & Birmingham, Al. (2011)
The 1948 Tinker Air Force Base tornadoes were two tornadoes which struck Tinker Air Force Base in Oklahoma City, Oklahoma, on March 20 and 25, 1948. Both are estimated to have been equivalent to F3 in intensity on the modern Fujita scale of tornado intensity, which was not devised until 1971. The March 20 tornado was the costliest tornado in Oklahoma history at the time. On March 25, meteorologists at the base noticed the extreme similarity between the weather conditions of that day and March 20, and later in the day issued a "tornado forecast", which was verified when a tornado struck the base that evening. This was the first official tornado forecast, as well as the first successful tornado forecast, in recorded history.2011 Tuscaloosa–Birmingham tornado
The 2011 Tuscaloosa–Birmingham tornado was a large and violent EF4 multiple-vortex tornado that devastated portions of Tuscaloosa and Birmingham, Alabama, as well as smaller communities and rural areas between the two cities, during the late afternoon and early evening of Wednesday, April 27, 2011. It is one of the costliest tornadoes on record. It was one of the 360 tornadoes in the 2011 Super Outbreak, the largest tornado outbreak in United States history. The tornado reached a maximum path width of 1.5 miles (2.4 km) during its track through Tuscaloosa, and once again when it crossed Interstate 65 north of Birmingham, and attained estimated winds of 190 mph (310 km/h) shortly after passing through the city. It then went on to impact parts of Birmingham as a high-end EF4 before dissipating. This was the third tornado to strike the city of Tuscaloosa in the past decade, and the second in two weeks.2013 El Reno tornado
The El Reno tornado was a very large EF3 tornado that occurred over rural areas of Central Oklahoma during the early evening of Friday, May 31, 2013. The widest tornado in recorded history, it was part of a larger weather system that produced dozens of tornadoes over the preceding days. The tornado initially touched down at 6:03 p.m. Central Daylight Time (2303 UTC) about 8.3 miles (13.4 km) west-southwest of El Reno, rapidly growing in size and becoming more violent as it tracked through central portions of Canadian County. Remaining over mostly open terrain, the tornado did not impact many structures; however, measurements from mobile weather radars revealed extreme winds up to 301 mph (484 km/h) within the vortex; these are the second-highest observed wind speeds on Earth, with only the 1999 Bridge Creek–Moore tornado having recorded slightly higher wind speeds. As it crossed U.S. Highway 81, it had grown to a record-breaking width of 2.6 miles (4.2 km). Turning northeastward, the tornado soon weakened. Upon crossing Interstate 40, the tornado dissipated around 6:43 p.m. CDT (2343 UTC), after tracking for 16.2 miles (26.1 km), it avoided affecting the more densely populated areas near and within the Oklahoma City metropolitan area.
The tornado killed four storm chasers, the first known deaths in the history of storm chasing. Although the tornado remained over mostly open terrain, dozens of storm chasers unaware of its immense size and erratic movement were caught off-guard. Near Highway 81, TWISTEX scientist and engineer Tim Samaras, along with his son Paul and research partner Carl Young, died in the tornado. Paul and Young were ejected from their Chevrolet Cobalt by the storm's sub-vortex, while Tim was still buckled in the passenger's seat. Local resident Richard Henderson, who decided to follow the storm, lost his life in that same area. He snapped a picture of the tornado from his cellular phone before it struck him. Other chasers, including Mike Bettes of The Weather Channel and Reed Timmer, were either injured or had their vehicles damaged. A Doppler on Wheels-based analysis of how the tornado impacted these teams revealed that they were hit by an intense internal sub-vortex. Overall, the tornado was responsible for eight fatalities and 151 injuries. The National Weather Service referred to the tornado as "the most dangerous tornado in storm observing history."Alongside rush hour traffic, thousands of residents in Oklahoma City attempted to outrun the storm by taking to the roads in an attempt to drive out of the tornado's projected path. By attempting to escape the storm by vehicle, in direct contrast to the recommended plan of action, residents put themselves at great risk from the storm; had the tornado maintained itself and passed over the congested freeways, more than 500 lives could have been lost.2013 Moore tornado
On the afternoon of Monday, May 20, 2013, a large and extremely powerful EF5 tornado ravaged Moore, Oklahoma, and adjacent areas, with peak winds estimated at 210 mph (340 km/h), killing 24 people (plus two indirect fatalities) and injuring 212 others. The tornado was part of a larger weather system that had produced several other tornadoes across the Great Plains over the previous two days, including five that 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 (19:46 UTC), and stayed on the ground for 37 minutes over a 17-mile (27 km) path, crossing through a heavily populated section of Moore. The tornado was 1.08 miles (1.74 km) wide at its peak. It followed a roughly similar track to the deadlier 1999 Bridge Creek–Moore tornado, which was smaller in size but just as severe; however, very few homes and neither of the stricken schools in the area had purpose-built storm shelters in the intervening years since the earlier tornado struck Moore.Cyclone Olivia
Severe Tropical Cyclone Olivia was a powerful cyclone that produced the highest non-tornadic winds on record on Barrow Island, 408 kilometres per hour (254 mph), breaking the record of 372 km/h (231 mph) on Mount Washington in the United States in April 1934. The 13th named storm of the 1995–96 Australian region cyclone season, Olivia formed on 3 April 1996 to the north of Australia's Northern Territory. The storm moved generally to the southwest, gradually intensifying off Western Australia. On 8 April, Olivia intensified into a severe tropical cyclone and subsequently turned more to the south, steered by a passing trough. On 10 April, Olivia produced the worldwide record strongest gust on Barrow Island, and on the same day the cyclone made landfall near Varanus Island. The storm quickly weakened over land, dissipating over the Great Australian Bight on 12 April.
While in its formative stages, Olivia produced light rainfall in the Northern Territory. While offshore Western Australia, the cyclone forced oil platforms to shut down, and the combination of high winds and waves caused heavy damage to oil facilities. Onshore, Olivia's high winds damaged several small mining towns, halting operations. Every house in Pannawonica sustained some damage. One person in the town was injured by flying glass and had to be flown to receive treatment, and nine others were lightly injured. The cyclone also produced heavy rainfall and a localized storm surge. Damage was estimated "in the millions". While the storm was dissipating, rough seas in South Australia killed A$60 million (US$47.5 million) worth of farm-raised tuna at Port Lincoln. The name Olivia was retired after the season.El Reno, Oklahoma
El Reno is a city in and county seat of Canadian County, Oklahoma, United States. As of the 2010 census, the city population was 16,729. The city was begun shortly after the 1889 land rush and named for the nearby Fort Reno. It is located in the central part of the state, approximately 25 miles (40 km) west of downtown Oklahoma City, and is part of the Oklahoma City Metropolitan Statistical Area.Fujita scale
The Fujita scale (F-Scale), or Fujita–Pearson scale (FPP scale), is a scale for rating tornado intensity, based primarily on the damage tornadoes inflict on human-built structures and vegetation. The official Fujita scale category is determined by meteorologists and engineers after a ground or aerial damage survey, or both; and depending on the circumstances, ground-swirl patterns (cycloidal marks), weather radar data, witness testimonies, media reports and damage imagery, as well as photogrammetry or videogrammetry if motion picture recording is available. The Fujita scale was replaced with the Enhanced Fujita scale (EF-Scale) in the United States in February 2007. In April 2013, Canada adopted the EF-Scale over the Fujita scale along with 31 "Specific Damage Indicators" used by Environment Canada (EC) in their ratings.Hook echo
A hook echo is a pendant or hook-shaped weather radar signature as part of some supercell thunderstorms. It is found in the lower portions of a storm as air and precipitation flow into a mesocyclone resulting in a curved feature of reflectivity. The echo is produced by rain, hail, or even debris being wrapped around the supercell. It is one of the classic hallmarks of tornado-producing supercells. The National Weather Service may consider the presence of a hook echo coinciding with a tornado vortex signature as sufficient to justify issuing a tornado warning.List of F5 and EF5 tornadoes
Among the most violent known meteorological events are tornadoes. Each year, more than 2,000 tornadoes occur worldwide, with the vast majority occurring in the United States and Europe. In order to assess the intensity of these events, meteorologist Ted Fujita devised a method to estimate maximum winds within the storm based on damage caused; this became known as the Fujita scale. At the top end of the scale, which ranks from 0 to 5, are F5 tornadoes. These storms were estimated to have had winds between 260 mph (420 km/h) and 318 mph (512 km/h). Following two particularly devastating tornadoes in 1997 and 1999, engineers questioned the reliability of the scale. Ultimately, a new scale was devised that took into account 28 different damage indicators; this became known as the Enhanced Fujita scale. With building designs taken more into account, winds in an EF5 tornado were estimated to be in excess of 200 mph (320 km/h).Since 1950, there have been 59 officially rated F5 and EF5 tornadoes in the United States and 1 F5 in Canada. Additionally, the works of tornado expert Thomas P. Grazulis revealed the existence of several dozen more between 1880 and 1995. Grazulis also put into question the ratings of several currently rated F5 tornadoes. Outside the United States and Canada, seven tornadoes have been rated F5: two each in France, Germany, and Italy and one in Russia. Several other tornadoes are also documented as possibly attaining this status.
Since structures are completely destroyed in both cases, the identification and assignment of scale between an EF4 tornado and an EF5 is often very difficult.List of United States tornado emergencies
Since its first use in 1999, the National Weather Service (NWS) has used the Tornado Emergency bulletin, which is an enhanced form of a Tornado Warning used when a confirmed tornado poses a significant threat to life and property in a populated area. Below is a listing of all known tornado emergencies issued in the United States to date.List of tornadoes in the 1999 Oklahoma tornado outbreak
From May 2 to 8, 1999, a large tornado outbreak took place across much of the Central and parts of the Eastern United States, as well as southern Canada. During this week-long event, 152 tornadoes touched down in these areas. The most dramatic events unfolded during the afternoon of May 3 through the early morning hours of May 4 when more than half of these storms occurred. Oklahoma experienced its largest tornado outbreak on record, with 70 confirmed. The most notable of these was the F5 Bridge Creek–Moore tornado which devastated Oklahoma City and suburban communities. The tornado killed 36 people and injured 583 others; losses amounted to $1 billion, making it the first billion-dollar tornado in history. Overall, 50 people lost their lives during the outbreak and damage amounted to $1.4 billion.On May 2, a strong area of low pressure moved out of the Rocky Mountains and into the High Plains, producing scattered severe weather and ten tornadoes in Nebraska. The following day, atmospheric conditions across Oklahoma became significantly more favorable for an outbreak of severe weather. Wind profiles across the region strongly favored tornadic activity, with the Storm Prediction Center stating, "it became more obvious something major was looming" by the afternoon hours. Numerous supercell thunderstorms developed across the state as well as bordering areas in Kansas and Texas. Over the following 48 hours, May 3–4, 116 tornadoes touched down across the Central United States. Following the extensive outbreak, activity became increasingly scattered from May 5 to 8, with 26 tornadoes touching down across the Eastern United States and Quebec.Moore, Oklahoma tornado
Moore, Oklahoma tornado may refer to:
1999 Bridge Creek–Moore tornado
2003 Moore–Choctaw tornado
2010 Moore–Choctaw tornado
2013 Moore tornadoMultiple-vortex tornado
A multiple-vortex tornado is a tornado that contains several vortices (called subvortices or suction vortices) rotating around, inside of, and as part of the main vortex. The only times multiple vortices may be visible are when the tornado is first forming or when condensation and debris are balanced such that subvortices are apparent without being obscured. They can add over 100 mph to the ground-relative wind in a tornado circulation, and are responsible for most (if not all) cases where narrow arcs of extreme destruction lie right next to weak damage within tornado paths.Satellite tornado
A satellite tornado is a tornado that rotates around a larger, primary tornado and interacts with the same mesocyclone. Satellite tornadoes occur apart from the primary tornado and are not considered subvortices; the primary tornado and satellite tornadoes are considered to be separate tornadoes. The cause of satellite tornadoes is not known. Such tornadoes are more often anticyclonic than are typical tornadoes and these pairs may be referred to as tornado couplets. Satellite tornadoes most commonly form in association with very large and intense tornadoes.Satellite tornadoes are relatively uncommon. When a satellite tornado does occur there is often more than one orbiting satellite spawned during the life cycle of the tornado or with successive primary tornadoes spawned by the parent supercell (a process known as cyclic tornadogenesis and leading to a tornado family). On tornado outbreak days, if satellite tornadoes occur with one supercell, there is an elevated probability of their occurrence with other supercells.Satellite tornadoes may merge into their companion tornado although often the appearance of this occurring is an illusion caused when an orbiting tornado revolves around the backside of a primary tornado obscuring view of the satellite. During the March 1990 Central United States tornado outbreak, one member of a tornado family (rated F5) constricted and became a satellite tornado of the next tornado of the family before merging into the new primary tornado which soon also intensified to F5.Some examples of tornado couplets include the Tri-State Tornado, the Chickasha tornado during the 1999 Oklahoma tornado outbreak, the 2007 Greensburg tornado, and the 2013 El Reno tornado. Satellite tornadoes are more likely to be recognized in recent decades than in the far past as eyewitness accounts as well as damage survey information are often available for later events. The advent of storm chasing, in particular, boosts the likelihood that satellite tornadoes are noticed visually and/or on mobile radar. These tornadoes may remain over open country and thus cause less structural damage and consequently are less widely known. Such examples include near Beloit, Kansas on 15 May 1990 and during Project VORTEX near Allison, Texas on 8 June 1995, among other events.Severe weather terminology (United States)
This article describes severe weather terminology used by the National Weather Service (NWS) in the United States. The NWS, a government agency operating as an arm of the National Oceanic and Atmospheric Administration (NOAA) branch of the United States Department of Commerce (DoC), defines precise meanings for nearly all of its weather terms. This article describes NWS terminology and related weather scales used by the agency. Some terms may be specific to certain cities or regions.Tornado intensity
Tornado intensity can be measured by in situ or remote sensing measurements, but since these are impractical for wide scale use, intensity is usually inferred via proxies, such as damage. The Fujita scale and the Enhanced Fujita scale rate tornadoes by the damage caused. The Enhanced Fujita Scale was an upgrade to the older Fujita scale, with engineered (by expert elicitation) wind estimates and better damage descriptions, but was designed so that a tornado rated on the Fujita scale would receive the same numerical rating. An EF0 tornado will probably damage trees and peel some shingles off the roof. an EF5 tornado can rip homes off their foundations and leaving them bare and can even deform large skyscrapers. The similar TORRO scale ranges from a T0 for extremely weak tornadoes to T11 for the most powerful known tornadoes. Doppler radar data, photogrammetry, and ground swirl patterns (cycloidal marks) may also be analyzed to determine intensity and award a rating.
Tornadoes vary in intensity regardless of shape, size, and location, though strong tornadoes are typically larger than weak tornadoes. The association with track length and duration also varies, although longer track (and longer lived) tornadoes tend to be stronger. In the case of violent tornadoes, only a small portion of the path area is of violent intensity; most of the higher intensity is from subvortices. In the United States, 80% of tornadoes are EF0 and EF1 (T0 through T3) tornadoes. The rate of occurrence drops off quickly with increasing strength—less than 1% are violent tornadoes (EF4, T8 or stronger).Tornado outbreak of May 4–6, 2007
The tornado outbreak of May 4–6, 2007 was a major and damaging tornado outbreak that significantly affected portions of the Central United States. The most destructive tornado in the outbreak occurred on the evening of May 4 in western Kansas, where about 95% of the city of Greensburg in Kiowa County was destroyed by an EF5 tornado, the first of such intensity since the 1999 Bridge Creek–Moore tornado. The supercell killed 13 people, including 11 in Greensburg and two from separate tornadoes. At least 60 people were injured in Greensburg alone. It was the strongest tornado of an outbreak which included several other tornadoes reported across Oklahoma, Colorado, Kansas and South Dakota that occurred on the same night.Although the most damaging tornado of the outbreak sequence occurred in Greensburg on the 4th, twenty-five tornadoes were confirmed that day. That number exploded to 84 the following day (May 5), with many tornadoes near the affected area from the previous night. Most were in open country, but there were injuries in at least two spots in Kansas, and one death reported near a county lake in Ottawa County. 14 more tornadoes were confirmed on May 6th in the region before the outbreak finally ended.Tornado records
This article lists various tornado records. The most "extreme" tornado in recorded history was the Tri-State Tornado, which spread through parts of Missouri, Illinois, and Indiana on March 18, 1925. It is considered an F5, even though tornadoes were not ranked on any scale at the time. It holds records for longest path length at 219 miles (352 km), longest duration at about 3½ hours, and fastest forward speed for a significant tornado at 73 mph (117 km/h) anywhere on Earth. In addition, it is the deadliest single tornado in United States history with 695 fatalities. It was also the third-costliest tornado in history at the time, but has been surpassed by several others non-normalized. When costs are normalized for wealth and inflation, it still ranks third today.The deadliest tornado in world history was the Daulatpur–Saturia tornado in Bangladesh on April 26, 1989, which killed approximately 1,300 people. In its history, Bangladesh has had at least 19 tornadoes kill more than 100 people, almost half of the total for the rest of the world.
For 37 years, the most extensive tornado outbreak on record, in almost every category, was the 1974 Super Outbreak, which affected a large area of the central United States and extreme southern Ontario in Canada on April 3 and April 4, 1974. Not only did this outbreak feature 148 tornadoes in only 18 hours, but an unprecedented number of them were violent; 7 were of F5 intensity and 23 were F4. During the peak of this outbreak there were 16 tornadoes on the ground at the same time. More than 300 people, possibly as many as 330, were killed by tornadoes during this outbreak. However, this record was later broken during the 2011 Super Outbreak, which resulted in 360 tornadoes and 324 tornadic fatalities.Wind speed
Wind speed, or wind flow velocity, is a fundamental atmospheric quantity caused by air moving from high to low pressure, usually due to changes in temperature. Note that wind direction is usually almost parallel to isobars (and not perpendicular, as one might expect), due to Earth's rotation.
Wind speed affects weather forecasting, aviation and maritime operations, construction projects, growth and metabolism rate of many plant species, and countless other implications.Wind speed is now commonly measured with an anemometer, but can also be classified using the older Beaufort scale, which is based on personal observation of specifically defined wind effects.