Meteorological history | |
---|---|
Duration | March 11–13,1990 |
Tornado outbreak | |
Tornadoes | 64 (confirmed) |
Maximum rating | F5 tornado |
Highest winds | 300 mph (480 km/h) to 350 mph (560 km/h) |
Overall effects | |
Fatalities | 2 fatalities ≥89 injuries |
Damage | $543.4 million (1990 USD) $1.3 billion (2024 USD) |
Areas affected | Midwestern United States,United States Great Plains |
Part of the tornado outbreaks of 1990 |
The March 1990 Central United States tornado outbreak affected portions of the United States Great Plains and Midwest regions from Iowa to Texas from March 11 to March 13,1990. The outbreak produced at least 64 tornadoes across the region,including four violent tornadoes;two tornadoes,which touched down north and west of Wichita,Kansas,were both rated F5,including the tornado that struck Hesston. In Nebraska,several strong tornadoes touched down across the southern and central portion of the state,including an F4 tornado (possibly a family of tornadoes) that traveled for 131 miles (211 km) making it the longest tracked tornado in the outbreak. Two people were killed in the outbreak,one each by the two F5 tornadoes in Kansas.
On March 12,upper-air maps indicated a high-pressure area situated over the Southeastern United States and a closed low-pressure area and accompanied trough entrenched across western portions of the country. Southwesterly flow across the Rocky Mountains proved favorable for low-level lee cyclogenesis,and surface analyses late on March 12 depicted the formation of a 1,004 millibars (29.65 inHg) low-pressure area over eastern Colorado. In the lower levels of the atmosphere,a low-level jet stretching from southern Texas into Iowa invigorated the northward transport of moisture from the Gulf of Mexico. The moisture became entrenched in the warm sector of the low-pressure area,to the east of a well-defined dryline extending from western Kansas into western Texas. [1] Overnight on March 12 into the morning hours of March 13,widespread convection developed across Oklahoma and progressed northeastward into Kansas and Iowa,to the south of a quasi-stationary weather front,leaving a distinct outflow boundary across central and eastern Kansas. [2] Early on March 13,morning atmospheric soundings across the Great Plains indicated an increasingly volatile atmosphere,with warming surface temperatures,strengthening low-level wind fields,and veering winds aloft. A modified atmospheric profile near Hesston,Kansas,indicated convective available potential energy around 3,200 J/kg already in place at 12:00 UTC. [2] In general,weather researchers remarked that the overarching pattern on March 13,1990,was a synoptically evident pattern reminiscent of past tornado outbreaks. [2] The National Severe Storms Forecast Center –known in modern times as the Storm Prediction Center –responded to this pattern by issuing a broad Moderate risk for severe weather across a wide swath of the Great Plains. [3]
As the trough continued its approach from the west,upper-air plots showed enhanced diffluence focused across much of the region. Into the afternoon hours,the surface low deepened to 996 millibars (29.41 inHg) as it progressed into western Kansas and the Oklahoma panhandle. The increasing atmospheric pressure gradient associated with this feature continued to enhance convergence along the dryline,while the influence of warm daytime temperatures exceeding 70 °F (21 °C) pushed the dryline eastward into western Oklahoma. Continued southwesterly flow around the mid-level low over Utah,Wyoming,and Colorado advected cold mid-level temperatures northeastward toward Kansas,Oklahoma,and Texas. Steep mid-level lapse rates further contributed to destabilization of the atmosphere,while moisture content and vertical wind profiles continued to improve. Low-level winds out of the southeast by the evening of March 13 further contributed to convergence along the dryline,which would become the focal point for several tornadic supercells over the ensuing hours as mid-level winds near 100 knots (120 mph;190 km/h) intersected the region. [1] [4] Additional supercells developed along the outflow boundary in Kansas,notably the Hesston tornado family. [2] Alongside the tornado outbreak in the warm sector of the low-pressure area,seasonally cold air on the backside of the low contributed to severe wintry weather,with snowfall up to 8 inches (200 mm) and blizzard-like conditions reported across the Nebraska panhandle. [5]
FU | F0 | F1 | F2 | F3 | F4 | F5 | Total |
---|---|---|---|---|---|---|---|
0 | 12 | 25 | 13 | 10 | 2 | 2 | 64 |
(based on NOAA Storm Data)
F# | Location | County | Time (UTC) | Path length | Damage | |
---|---|---|---|---|---|---|
Kansas | ||||||
F0 | N of Plevna | Reno | 2300 | 0.1 miles (160 m) | ||
F1 | Alder to S of Geneseo | Rice | 2315 | 14 miles (23 km) | ||
Sources:NOAA Storm Data Tornado History Project - Storm Data,March 11,1990 |
F# | Location | County | Time (UTC) | Path length | Damage | |
---|---|---|---|---|---|---|
Iowa | ||||||
F0 | NW of Sawyer | Lee | 0440 | 0.2 miles (0.32 km) | ||
Kansas | ||||||
F1 | SE of Topeka | Shawnee,Douglas | 0549 | 5 miles (8.0 km) | Rated F2 by Grazulis. | |
F1 | W of McClouth | Jefferson | 0610 | 3 miles (4.8 km) | ||
Sources:NOAA Storm Data Tornado History Project - Storm Data - March 12,1990 |
F# | Location | County | Time (UTC) | Path length | Damage | |
---|---|---|---|---|---|---|
Kansas | ||||||
F1 | NW of Jetmore | Hodgeman | 0836 | 1 mile (1.6 km) | ||
F5 | Castleton to Hesston | Reno,Harvey,McPherson | 2234 | 48 miles (77 km) | 1 death - See section on this tornado | |
F1 | E of Thornburg | Smith | 2248 | 13 miles (21 km) | ||
F1 | NE of Esbon | Jewell | 2300 | 1.5 miles (2.4 km) | ||
F5 | Goessel to NE of Hillsboro | Harvey,McPherson,Marion | 2330 | 22.0 miles (35.4 km) | 1 death - See section on this tornado | |
F0 | SW of Portland | Sumner | 0004 | 0.1 miles (160 m) | ||
F0 | N of Conway Springs | Sumner | 0012 | 0.1 miles (160 m) | ||
F2 | W of Pilsen to NW of Volland | Marion,Morris,Geary,Wabaunsee | 0015 | 55 miles (89 km) | See section on this tornado | |
F1 | SW of Webber | Jewell | 0020 | 5 miles (8.0 km) | ||
F1 | S of Danville | Harper | 0035 | 12 miles (19 km) | ||
F1 | E of Randall | Jewell,Cloud,Republic | 0045 | 13 miles (21 km) | ||
F3 | W of Moundridge | Reno,Harvey,McPherson | 0055 | 18 miles (29 km) | A farm and three homes were destroyed. Caused $275,000 in damage. | |
F2 | W of Belleville | Republic | 0100 | 15 miles (24 km) | Several farmhouses sustained extensive damage. | |
F0 | S of Belleville | Republic | 0116 | 0.5 miles (0.80 km) | ||
F0 | Salina | Saline | 0150 | 0.2 miles (320 m) | ||
F1 | E of Wamego | Pottawatomie | 0203 | 2 miles (3.2 km) | ||
F0 | S of Concordia | Cloud | 0240 | 0.2 miles (320 m) | ||
F1 | S of Chetopa | Labette | 0645 | 2 miles (3.2 km) | ||
Iowa | ||||||
F1 | N of Stiles to SE of Floris | Davis | 2132 | 14 miles (23 km) | ||
F0 | Bettendorf area | Scott | 2231 | 0.3 miles (480 m) | ||
F0 | E of LeClaire | Scott | 2242 | 0.2 miles (320 m) | ||
F3 | E of LeClaire to SE of Albany,IL | Scott,Rock Island (IL),Whiteside (IL) | 2245 | 15.5 miles (24.9 km) | Multiple-vortex tornado caused major damage in the Cordova and Port Byron areas. 12 homes were heavily damaged or destroyed,and 26 others sustained lesser damage. One man broke his leg when he was blown off of a scaffold at Cordova Nuclear Plant. | |
F4 | Prairieburg to Worthington | Linn,Jones,Delaware,Dubuque | 2253 | 19 miles (31 km) | In Worthington,39 homes and businesses were damaged or destroyed. 13 farms were destroyed as well. Tornado was a half-mile wide at times. | |
F1 | NE of LeClaire | Scott,Clinton | 2242 | 13 miles (21 km) | ||
F1 | Monticello area | Jones | 2308 | 6 miles (9.7 km) | ||
F1 | NE of Crescent | Pottawattamie | 2242 | 8 miles (13 km) | ||
F1 | S of Holy Cross | Dubuque | 2355 | 3 miles (4.8 km) | ||
F0 | NE of Ortonville | Dallas | 0120 | 0.1 miles (160 m) | ||
F2 | Ogden to E of Stanhope | Boone,Hamilton | 0125 | 22 miles (35 km) | Tornado killed livestock and destroyed several outbuildings. Caused $616,000 in damage. | |
F1 | E of Ridgeport | Boone | 0135 | 1 mile (1.6 km) | ||
F2 | Ankeny to S of Maxwell | Polk,Story | 0155 | 15 miles (24 km) | Rain-wrapped tornado severely damaged 20 homes in Ankeny,with 16 others sustaining lesser damage. A condominium lost part of its roof,which was thrown onto I-35,resulting in a major car accident. At least a dozen other cars were blown off of the interstate by the tornado. Caused $2,000,000 in damage and injured 15 people. | |
F3 | E of Fernald | Story | 0236 | 9 miles (14 km) | A tractor-trailer was lifted and thrown into a ditch,injuring the driver. Multiple buildings were damaged or destroyed at a farm as well. Rated F2 by Grazulis. | |
Oklahoma | ||||||
F2 | NW of Bradley to E of Norman | Grady,McClain,Cleveland | 2244 | 28 miles (45 km) | Two mobile homes were destroyed and frame homes were damaged near the beginning of the path. The tornado crossed into McClain County and destroyed eight additional mobile homes before clipping the north side of Washington,destroying a trailer and the second story of a house. The tornado then struck Noble before dissipating. In Noble,multiple homes sustained roof and structural damage,and an apartment building lost part of its roof. Tractor-trailers and a mobile home were overturned. The high school lost its press box,scoreboard,and several light poles. One person was injured. | |
F3 | SE of Hawley to NE of Wakita | Grant | 2315 | 19 miles (31 km) | One house sustained major damage and another lost its roof. | |
F2 | W of Criner to W of Slaughterville | McClain,Cleveland | 2331 | 18 miles (29 km) | Trailers and outbuildings were damaged and many trees were uprooted. Rated F1 by Grazulis. | |
F1 | NE of Norman | Cleveland | 2353 | 5 miles (8.0 km) | ||
F3 | NE of Wakita to SW of Mayfield,KS | Grant,Sumner (KS) | 2354 | 22 miles (35 km) | Caused tree damage in Oklahoma before crossing into Kansas,where five homes were damaged. | |
F2 | SW of Stella to SE of Jacktown | Cleveland,Pottawatomie,Lincoln | 2359 | 19 miles (31 km) | At the beginning of the path,a mobile home was destroyed in Stella,resulting in a serious injury. A barn was destroyed,a house was unroofed,and three trailers were damaged elsewhere along the path. A mobile home was destroyed near Meeker before the tornado dissipated. | |
F1 | W of Waurika to SW of Loco | Jefferson,Stephens | 0001 | 21 miles (34 km) | ||
F3 | SW of Loco to NW of Alpers | Jefferson,Stephens,Carter,Garvin | 0058 | 22 miles (35 km) | Tornado caused major damage in and around Ratliff City. Five mobile homes were destroyed and a motor home was rolled 100 feet. A five-ton crane was blown over,several vehicles were damaged,and debris was found up to a mile away. Caused $750,000 in damage and injured one person. | |
F2 | NE of Tatums to NE of Paul's Valley | Garvin | 0150 | 28 miles (45 km) | In Pauls Valley,a farm implement company had its roof torn off,and a civic club building lost part of its roof. Barns were destroyed outside of town as well. | |
F2 | NE of Edna | Creek,Okmulgee | 0210 | 9 miles (14 km) | Several barns were destroyed and 14 power poles were snapped. Caused $75,000 in damage. | |
Nebraska | ||||||
F1 | NW of Shelton | Buffalo | 2245 | 1 mile (1.6 km) | ||
F3 | NW of Minden to S of Cairo | Kearney,Buffalo,Hall | 2300 | 32 miles (51 km) | Numerous outbuildings were destroyed,trees were uprooted,and a county bridge was destroyed. Five farmsteads were heavily damaged as well. | |
F4 | S of Red Cloud to E of Schuyler | Webster,Nuckolls,Clay,Fillmore,York,Seward,Butler,Colfax | 2305 | 131 miles (211 km) | This was either an extremely long-tracked tornado or a tornado family. Near Red Cloud,a farmhouse was completely "wiped out". The tornado moved into Nuckolls County and struck Lawrence,where 8 homes were destroyed and 45 others were damaged. Crossing into Clay County,the tornado struck Sutton,where one business was destroyed and 11 others were damaged. 49 homes in Sutton were damaged,and a truck and a police car were flipped. 20 farms were damaged in rural areas nearby. The tornado downed trees and power lines in Fillmore County before crossing into York County. A farmhouse was destroyed near McCool Junction. South of York,the tornado destroyed another farmhouse,heavily damaged a gas station and convenience store,tore the roof off of a motel,and destroyed two trucks. A dozen farms were damaged in York County,and about 10,000 geese were killed. 57 railroad cars were derailed near Waco before the tornado crossed into Seward County,where trees and power lines were damaged. The tornado then crossed into Butler County and passed near David City,impacting numerous farmsteads. 35 homes and 155 other structures were damaged or destroyed near David City,and about 1,200 livestock were killed or injured. The tornado then moved into Colfax County,damaging four farms near Schuyler before dissipating. A total of nine people were injured. | |
F2 | E of Sacramento | Kearney | 2320 | 8 miles (13 km) | Several farms sustained extensive damage with livestock killed,and outbuildings and irrigation pivots destroyed. | |
F2 | S of Wood River | Adams,Hall | 2325 | 9 miles (14 km) | Two farms were hit,with a farmhouse sustaining extensive damage at one of them. Outbuildings,grain bins,and two barns were destroyed. | |
F0 | N of Kearney | Buffalo | 2335 | 0.1 miles (160 m) | ||
F3 | N of Alda to NW of Archer | Hall,Howard,Merrick | 2344 | 27 miles (43 km) | Five mobile homes were destroyed,and other homes sustained minor damage. 15 train cars were derailed near an Army Ordnance Plant,and 47 others were derailed near Grand Island. Several farms were damaged,some extensively with loss of cattle. | |
F2 | W of Fullerton | Merrick,Nance | 0023 | 13 miles (21 km) | Ten farms were damaged,with farmhouses damaged at four of them. | |
F1 | NE of Boone | Boone | 0025 | 1.5 miles (2.4 km) | ||
F1 | SE of Fullerton | Nance | 0030 | 2 miles (3.2 km) | ||
F1 | Newman Grove area | Madison | 0045 | 0.2 miles (320 m) | ||
F1 | SE of Battle Creek | Madison | 0130 | 0.6 miles (0.97 km) | ||
F3 | N of Carleton to SE of Exeter | Thayer,Fillmore | 0145 | 25 miles (40 km) | A large hog facility and outbuildings were destroyed. A mobile home was destroyed as well. Rated F2 by Grazulis. | |
F3 | NE of Chester | Thayer | 0145 | 13 miles (21 km) | Tornado clipped Chester,where trees,outbuildings and propane tanks were damaged. Several farmsteads were damaged outside of town as well. Rated F2 by Grazulis. | |
F1 | N of Bancroft | Thurston | 0401 | 1.5 miles (2.4 km) | ||
Texas | ||||||
F0 | NE of Lusk | Throckmorton | 2330 | 0.2 miles (320 m) | ||
Missouri | ||||||
F2 | SE of Pleasant Hope | Polk | 0330 | 2 miles (3.2 km) | Five homes and 16 barns were damaged. | |
Sources:NOAA Storm Data Tornado History Project Storm Data - March 13,1990 [6] |
Tornado family | |
---|---|
Tornadoes | 3 |
Maximum rating | F5 tornado |
Highest winds | 300 mph (480 km/h) to 350 mph (560 km/h) |
Overall effects | |
Casualties | 2 fatalities,≥59 injuries |
Areas affected | Central Kansas |
Part of the tornado outbreaks of 1990 |
The F5 tornadoes that struck Hesston and Goessel were both spawned by the same supercell thunderstorm. They were part of what is known as a tornado family;a family that included several additional touchdowns after the Goessel storm dissipated. [7]
The first tornado of the Hesston storm touched down at approximately 4:34 p.m. CDT just to the northeast of Pretty Prairie. It was initially between 200 and 500 yards in diameter,and caused minimal (F1-F2) damage as it churned between Castleton and the Cheney Reservoir. Photographic evidence suggests significant widening as the tornado approached Haven and the Arkansas River. The damage path ranged between 1/2 and 3/4 miles near Haven,and several homes were completely demolished indicating F4 damage. Had the tornado moved through a more populated area in this stage of its life,it is likely that it would have caused much more dramatic damage. Fairly constant F3 damage was produced from Haven to Burrton and to the Little Arkansas River. The path width remained over 0.5 miles (0.80 km) in diameter.
Northeast of the Little Arkansas,the track abruptly decreased in width from 0.5 miles (0.80 km) to just over 300 yards (270 m). Photographs suggest what appears to be a re-organization of the tornadic circulation;initially a wedge like appearance,the funnel quickly became tall and narrow. The most significant damage was done in this stage,however. The tornado plowed into the town of Hesston,just northwest of Newton on I-135. A total of 226 homes and 21 businesses were destroyed,and several were swept completely from their foundations with only slabs and empty basements remaining. A few of the homes were anchor-bolted to their foundations. Several industrial buildings were also obliterated,trees in town were completely shredded,and vehicles were thrown and severely mangled or stripped down to their frames. Portions of the damage path in Hesston were rated F5. 20 farms were torn apart in rural areas outside of town. Light debris from Hesston was found 115 miles (185 km) away in Nebraska. One person died and 59 people were injured.
The series of events that occurred as the tornado moved past the Hesston area were most interesting. Eyewitness accounts observed the touchdown of an additional tornado just to the north. This is consistent with models of what is known as a "tornado handoff",in which an old mesocyclone and tornado occlude as a new mesocyclone and tornado further downwind becomes dominant. [8] Over the course of a few miles,the new tornado intensified and the original one abruptly constricted and apparently became a satellite tornado to the new tornado. Eventually,the Hesston tornado (after traveling nearly 48 miles (77 km)) occluded and merged with the new tornado,and the supercell began to re-intensify. The new tornado rapidly became very large,and violent damage was produced by the second tornado in Marion County. Several homes were again obliterated and completely swept away. An elderly woman was killed when the tornado cleanly swept away her army barracks that was converted into a home,but without a basement. The tornado produced very severe cycloidal ground scouring in farm fields,and damage near the town of Goessel was "extreme F5" according to NWS damage surveyors. The severity of the damage left behind by this tornado led some meteorologists to believe that the Goessel tornado was among the strongest ever documented at that time. The storm passed Goessel,clipped the northwestern portion of Hillsboro,then dissipated just NE of Risley,approximately 22 miles (35 km) from its genesis. [9] [10] [11]
The same supercell would produce another long-tracked F2 tornado that damaged many farms and destroyed four homes on the southern side of Dwight.
From April 26 to 27,1991,multiple supercells across Oklahoma and Kansas led to a regional tornado outbreak. Forced by a potent trough and focused along a dryline,these distinct thunderstorms moved northeast through a moist and highly unstable environment. A total of 55 tornadoes were confirmed,many of which were strong,F2 or greater on the Fujita scale. A widely documented F5 tornado tore through Andover,Kansas,killing 17 people. Additional fatalities occurred from significant tornadoes in other portions of Kansas and Oklahoma,with 21 deaths recorded in total. An F4 tornado was detected by a mobile doppler weather radar team which observed winds up to 270 mph (430 km/h) at the top of the funnel,the first time winds of F5 intensity were measured by radar,and the highest winds recorded by radar at the time. A news team filming an F2 tornado sought shelter under a Kansas Turnpike overpass,causing a misconception that overpasses can provide adequate shelter during a tornado. This outbreak occurred within a transition period for the National Weather Service and proved the value of NEXRAD radars,which were utilized in Oklahoma to provide advanced warning to residents.
The tornado outbreak sequence of March 1913 was a devastating series of tornado outbreaks that affected the northern Great Plains,the Southern United States,and sections of the upper Midwest over a two-day-long period between March 21–23,1913. Composed of two outbreaks,the sequence first began with a tornado outbreak that commenced in Mississippi early on March 21. Several significant tornadoes occurred,one of which killed seven people in one family and another destroyed much of Lower Peach Tree,Alabama,with 27 deaths all in that town. The tornado at Lower Peach Tree is estimated to have been equivalent to a violent F4 tornado on the Fujita scale,based upon damage accounts. The tornadoes occurred between 0630 and 1030 UTC,or pre-dawn local time,perhaps accounting for the high number of fatalities—a common trend in tornadoes in the Dixie Alley. In all,tornadoes in Mississippi,Georgia,and Alabama killed 48 people,perhaps more,that day and injured at least 150 people.
The 1996 Oakfield tornado outbreak was a severe weather event that occurred on July 18,1996,in Wisconsin,United States,primarily affecting the village of Oakfield. The outbreak produced 12 tornadoes,with the most significant being an F5 tornado which caused severe damage to the village and the surrounding areas. As of the present,this remains the most recent EF/F5 tornado to have occurred in the United States outside the peak months of April and May. No deaths were associated with the outbreak,with 17 injuries in total.
From May 19–22,1957,a tornado outbreak took place across the US Central Plains. A total of 59 tornadoes were reported from Colorado to the Mississippi Valley. The most destructive tornado of the severe weather event—likely part of a long-lived family—was rated at F5,the highest level,and is often called the Ruskin Heights tornado,after the site of its worst damage,a suburb and housing development in southern Kansas City,Missouri. Additionally,a powerful F4 tornado virtually destroyed Fremont,Missouri,claiming seven lives,and an F3 tornado killed eight others in and near Belgrade,Missouri. A pair of F4s—one in Minnesota,the other in Kansas—also neared F5 intensity. In all,59 people were killed during the outbreak,including 44 in the Ruskin Heights tornado.
A tornado family is a series of tornadoes spawned by the same supercell thunderstorm. These families form a line of successive or parallel tornado paths and can cover a short span or a vast distance. Tornado families are sometimes mistaken as a single continuous tornado,especially prior to the 1970s. Sometimes the tornado tracks can overlap and expert analysis is necessary to determine whether or not damage was created by a family or a single tornado. Oftentimes,tornadoes are small and don’t make it far before dying out. However,large tornadoes are also present in many situations that track for very long distances. To determine the average track length of a tornado,both of these factors must be taken into account. The track length of a tornado can be as short as a few feet to over 100 miles,thus making the average track length for a typical tornado about 1–2 miles. In some cases,such as the Hesston-Goessel,Kansas tornadoes of March 1990,different tornadoes of a tornado family merge,making discerning whether an event was continuous or not more difficult.
From May 4–6,2007,a major and damaging tornado outbreak 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 the new Enhanced Fujita Scale and 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.
This page documents notable tornadoes and tornado outbreaks worldwide in 2008. Strong and destructive tornadoes form most frequently in the United States,Bangladesh,and Eastern India,but they can occur almost anywhere under the right conditions. Tornadoes also develop occasionally in southern Canada during the Northern Hemisphere's summer and somewhat regularly at other times of the year across Europe,Asia,and Australia. Tornadic events are often accompanied with other forms of severe weather,including strong thunderstorms,strong winds,and hail.
The Tornado outbreak of June 7–8,1984 was a significant severe weather and tornado event that took place across the central United States from North Dakota to Kansas on June 7–8,1984. The tornado outbreak produced several significant tornadoes including an F5 tornado which traveled through Barneveld,Wisconsin,in the early hours of June 8,1984. The entire outbreak killed at least 13 people across three states including 9 in Barneveld alone.
A satellite tornado is a tornado that revolves 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 commonly occur in association with very powerful,large,and destructive tornadoes,indicative also of the strength and severity of the parent supercell thunderstorm.
A multi-day tornado outbreak affected the central plains of the United States from May 22–27,2008. It was also one of the largest continuous tornado outbreaks on record. A total of 173 tornadoes were confirmed,with the most intense activity occurring across the Great Plains. One person was killed when a large wedge tornado struck Windsor,Colorado,and two more deaths were reported in Pratt County,Kansas. One person was also killed near Hugo,Minnesota on May 25 and nine were killed by an EF5 tornado that destroyed most of Parkersburg,Iowa and a small subdivision of New Hartford,Iowa. Another fatality,caused by lightning related to the storms,occurred in central Kansas.
The March 2009 tornado outbreak sequence was a series of tornado outbreaks which affected large portions of the Central,Southern,and Eastern United States from March 23 to March 29. A total of 56 tornadoes touched down during the event,two of which were rated as EF3.
From May 3 to May 11,2003,a prolonged and destructive series of tornado outbreaks affected much of the Great Plains and Eastern United States. Most of the severe activity was concentrated between May 4 and May 10,which saw more tornadoes than any other week-long span in recorded history;335 tornadoes occurred during this period,concentrated in the Ozarks and central Mississippi River Valley. Additional tornadoes were produced by the same storm systems from May 3 to May 11,producing 363 tornadoes overall,of which 62 were significant. Six of the tornadoes were rated F4,and of these four occurred on May 4,the most prolific day of the tornado outbreak sequence;these were the outbreak's strongest tornadoes. Damage caused by the severe weather and associated flooding amounted to US$4.1 billion,making it the costliest U.S. tornado outbreak of the 2000s. A total of 50 deaths and 713 injuries were caused by the severe weather,with a majority caused by tornadoes;the deadliest tornado was an F4 that struck Madison and Henderson counties in Tennessee,killing 11. In 2023,tornado expert Thomas P. Grazulis created the outbreak intensity score (OIS) as a way to rank various tornado outbreaks. The tornado outbreak sequence of May 2003 received an OIS of 232,making it the fourth worst tornado outbreak in recorded history.
The 1999 Bridge Creek–Moore tornado was a large,long-lived and exceptionally powerful F5 tornado in which the highest wind speeds ever measured globally was recorded at 321 miles per hour (517 km/h) by a Doppler on Wheels (DOW) radar. Considered the strongest tornado ever recorded to have affected the metropolitan area,the tornado devastated southern portions of Oklahoma City,Oklahoma,United States while near peak intensity,along with surrounding suburbs and towns to the south and southwest of the city during the early evening of Monday,May 3,1999. Parts of Bridge Creek were rendered unrecognizable. The tornado covered 38 miles (61 km) during its 85-minute existence,destroying thousands of homes,killing 36 people,and leaving US$1 billion in damage,ranking it as the fifth-costliest on record not accounting for inflation. Its severity prompted the first-ever use of the tornado emergency statement by the National Weather Service.
From April 13 to 16,2012,a major tornado outbreak occurred across a large portion of the Great Plains. The storms resulted in six tornado-related fatalities,all of which occurred as a result of a nighttime EF3 tornado that caused major damage in and around Woodward,Oklahoma. Numerous other tornadoes occurred,including a violent EF4 tornado that passed near Marquette,Kansas,and an EF3 that caused major damage in Wichita.
This page documents the tornadoes and tornado outbreaks of 2013. Strong and destructive tornadoes form most frequently in the United States,Bangladesh,Brazil and Eastern India,but they can occur almost anywhere under the right conditions. Tornadoes also appear regularly in neighboring southern Canada during the Northern Hemisphere's summer season,and somewhat regularly in Europe,Asia,and Australia.
A significant and destructive tornado outbreak that affected parts of the Midwestern United States and lower Great Plains in mid-May 2013. This event occurred just days after a deadly outbreak struck Texas and surrounding southern states on May 15. On May 16,a slow moving trough crossed the Rockies and traversed the western Great Plains. Initially,activity was limited to scattered severe storms;however,by May 18,the threat for organized severe thunderstorms and tornadoes greatly increased. A few tornadoes touched down that day in Kansas and Nebraska,including an EF4 tornado near Rozel,Kansas. Maintaining its slow eastward movement,the system produced another round of severe weather nearby. Activity significantly increased on May 19,with tornadoes confirmed in Oklahoma,Kansas,Iowa,Missouri,and Illinois. In Oklahoma,two strong tornadoes,one rated EF4,caused significant damage in rural areas of the eastern Oklahoma City metropolitan area;two people lost their lives near Shawnee. The most dramatic events unfolded on May 20 as a large EF5 tornado devastated parts of Moore,Oklahoma,killing 24 people. Thousands of structures were destroyed,with many being completely flattened. Several other tornadoes occurred during the day in areas further eastward,though the majority were weak and caused little damage.
The following is a glossary of tornado terms. It includes scientific as well as selected informal terminology.
The tornado outbreak of April 8–9,2015 was a relatively small but damaging outbreak of tornadoes that occurred in parts of the Great Plains and in the Midwestern United States. 27 tornadoes were confirmed during the two days,most of them weak,however a select few of them were powerful and damaging.
The tornado outbreak sequence of May 2019 was a prolonged series of destructive tornadoes and tornado outbreaks affecting the United States over the course of nearly two weeks,producing a total of 400 tornadoes,including 53 significant events (EF2+). Eighteen of these were EF3 tornadoes,spanning over multiple states,including Nebraska,Kansas,Texas,Missouri,Oklahoma,Indiana,Iowa,and Ohio,with additional tornadoes confirmed across a region extending from California to New Jersey. Two EF4 tornadoes occurred,one in Dayton,Ohio,and the other in Linwood,Kansas. Four tornadoes during this outbreak were fatal,causing a total of eight fatalities. The deadliest of these occurred on May 22 near Golden City,Missouri,where an EF3 tornado took three lives,including an elderly couple in their eighties. The damaging series of tornadoes that occurred in Indiana and Ohio on the evening of May 27 during this event is sometimes locally referred to as the Memorial Day tornado outbreak of 2019,which became the fourth costliest weather event in Ohio history. The near continuous stream of systems also produced to widespread flash and river flooding,along with damaging winds and large hail.
A deadly and destructive outbreak sequence of 23 tornadoes struck parts of the Great Plains and the Great Lakes in late-June 1957. At least seven significant tornadoes (F2+) touched down during the outbreak sequence. The most devastating storm was a large,violent,and catastrophic 500-yard-wide F5 tornado family that struck Fargo,North Dakota on Thursday,June 20,1957,killing 10 people and becoming the deadliest tornado ever recorded in North Dakota. The outbreak caused 11 fatalities,105 injuries,and $25.883 million in damage.
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