Meteorological history | |
---|---|
Date | May 27,1997 |
Formed | May 27,1997,3:40 pm. CDT (UTC−05:00) |
Dissipated | May 27,1997,3:53 pm. CDT (UTC−05:00) |
Duration | 13 minutes |
F5 tornado | |
on the Fujita scale | |
Highest winds | >261 mph (420 km/h) |
Overall effects | |
Fatalities | 27 |
Injuries | 12 |
Damage | $40 million [1] (1997 USD) |
Areas affected | Jarrell,Texas and areas near Prairie Dell,Texas |
[2] | |
Part of the 1997 Central Texas tornado outbreak and tornadoes of 1997 |
On May 27,1997,a large tornado would produce catastrophic damage across portions of the Jarrell,Texas area. The tornado killed 27 residents of the town,many in a single subdivision,and inflicted approximately $40 million (1997 USD) in damages in its 13-minute,5.1 miles (8.2 km) track. It occurred as part of a tornado outbreak across central Texas;it was produced by a supercell that had developed from an unstable airmass and favorable meteorological conditions at the time,including high convective available potential energy (CAPE) values and warm dewpoints.
Several weaker tornadoes prior to the Jarrell tornado touched down and inflicted damage in nearby areas,particularly in Travis and Williamson counties. The Fort Worth branch of the National Weather Service issued several tornado watches and warnings as a result,and later issued a tornado warning for the area encompassing Jarrell as the tornado-producing supercell approached the town. Shortly thereafter,within the Williamson County line,the tornado touched down as an indistinct multi-vortex swathed in dust,which then strengthened rapidly as its width grew. As the tornado moved through a neighborhood near Jarrell,it began to slow down,before stopping completely over the area while reaching its maximum width and retaining intense winds. The tornado stalled over the neighborhood for approximately 3 minutes,producing some of the most extreme tornadic wind damage ever recorded. As the tornado left the subdivision,it began to weaken,before dissipating in a forested area. In total 27 residents of Jarrell,as well as hundreds of cattle,were killed. The tornado left behind a path of devastation,including multiple buildings swept off of their foundations.
As of 2024,this tornado is Texas' most recent F5 or EF5 tornado. The tornado was the fourth-deadliest of the 1990s in the United States,only being surpassed by the 1990 Plainfield tornado that killed 29,the 1998 Birmingham tornado that killed 32,and the 1999 Bridge Creek–Moore tornado that killed 36. It was the only F5 tornado of 1997,and the next F5-rated tornado would occur on April 8 of the following year.
On the morning of May 27, 1997, an upper-level low-pressure area located over portions of South Dakota and Nebraska had moved northward which caused a weak, mid-level flow across Texas. While this occurred, a cold front extended southwest of a surface-based low-pressure area from Fayetteville, Arkansas to the Dallas–Fort Worth metroplex (DFW) to the Permian Basin, which also included two decaying outflow boundaries northeast of the DFW metroplex. A gravity wave was also noted from the cold front near Waco, Texas and southward, which would promote initiation of supercells, including the one which produced the Jarrell tornado. [3] The latter two factors were caused by an overnight mesoscale convective system which had dissipated before the mesoscale setup of the Jarrell tornado. [4]
An upper-air balloon sounding was conducted by the National Weather Service in Fort Worth while the cold front passed directly over the DFW metroplex, which showed favorable mid-level lapse rates, a dewpoint temperature of 73 °F (23 °C) on the surface, and some wind shear, though not towards the surface, which suggested non-tornadic supercell activity. However, a sounding launched from Calvert, Texas a few hours later revealed surface-based convective available potential energy (CAPE) values above 6500 j/kg, up from 3000 j/kg shown by the sounding previously launched over the DFW metroplex. [3] This, along with extremely high CAPE values shown near the surface from a sounding over Waco at 12:00 CDT (17:00 UTC), likely caused vorticity near and along the cold front and the production of the Jarrell tornado. [3]
The supercell that produced the Jarrell tornado first developed in McLennan County before noon, initially moving slowly southwestward in the unstable airmass. [3] Shortly thereafter, a tornado watch was issued by the Storm Prediction Center for eastern Texas and western Louisiana. As the thunderstorm cell moved parallel to Interstate 35, it rapidly intensified and prompted the issuance of a severe thunderstorm warning for portions of McLennan County at 12:50 CDT (17:50 UTC), later being upgraded to a tornado warning as the supercell then began to rapidly exhibit lower-levels of rotation. [3] This would result in multiple tornadoes being produced before the Jarrell tornado occurred; most notably an F3 tornado which caused severe damage in portions of Falls County near Bruceville-Eddy and Lake Belton. [3] Another tornado, rated an F0, touched down near Stillhouse Dam and was incorrectly claimed as the Jarrell tornado due to its close proximity from the F5 tornado's path. [5]
Shortly thereafter, the supercell began to move slightly westward towards Jarrell and Salado while continuing to show signs of rapid, low-level rotation. This would result in another tornado warning being issued by the National Weather Service in Austin/San Antonio for Williamson County, including Jarrell, at 15:30 CDT (22:30 UTC), in response to the storm's approach to the town. The warning was in effect for a duration of one hour, and local warning sirens in the town went off an estimated 10–12 minutes before the impact. [3] [6] [7] Multiple short-lived, small, and rope-like funnel clouds preceded the Jarrell tornado; and despite being theorized and commonly accepted as being separate tornadoes, there is a possibility that these were part of it. [5] Additionally, some reports stated an F1 tornado near Prairie Dell as an earlier continuation of this tornado. [5]
The tornado officially touched down within the Williamson County line 3 miles (4.8 km) north of Jarrell as a faint, drill-bit funnel wrapped in large amounts of dust at 3:40 pm CDT (20:40 UTC). The tornado began to undergo a rapid intensification as it took on a multi-vortex shape. [8] [5] Traffic along Interstate 35 came to a stop as the tornado descended nearby; [9] the Texas Highway Patrol also stopped traffic on both sides of the interstate under the expectation that the tornado would cross the highway. However, it instead moved parallel to Interstate 35 without impacting the roadway. [10]
Tracking south-southwest, the tornado quickly intensified and grew in width. [3] The exact size of the tornado was difficult to determine during this portion of the tornado's life. Its intense winds scoured the ground, vegetation, and stripped pavement from three county roads; the thickness of the asphalt pavement was an estimated 3 inches (7.6 cm). [11] A culvert plant near the intersection of two county roads collapsed. Nearby, a similar plant and a mobile home sustained some damage, with the latter struck by a 2×4'' piece of lumber. [5] Some of the most extreme damage nearby was inflicted to a small metal-framed recycling plant that was directly hit and destroyed, with only several twisted and bent metal beams remaining. [8] Multiple people were sheltering in a mobile home far south of the recycling plant, but later decided to evacuate to a frame house to take cover. The frame house was directly hit by the tornado moments later, killing everyone inside, while the mobile home only sustained minor damage. [3]
The tornado turned slightly, entering the Double Creek Estates at F5 intensity. [8] It grew to its maximum width, estimated to be 3⁄4 mile (1.2 km). Post-event surveys and eyewitness accounts suggested that the tornado began to slow its pace, contributing to the extremely violent damage observed there. [3] [12] The tornado immediately began to destroy structures and homes as it hit multiple smaller streets at the northeastern edge of the Estates. The exact time of this is unknown, but timekeeping devices from remaining debris and synced videos had the tornado's starting impact at most likely 3:48 pm. [11] [8]
The entire neighborhood of Double Creek Estates was subject to extreme winds for three minutes due to the "stalling" pattern of the tornado, which likely exacerbated the damage. Multiple homes on Double Creek Drive were destroyed, [5] with foundations in the direct path of the tornado having their plumbing and sill plates ripped away. [13] There were 38 structures in Double Creek Estates that were destroyed; three businesses adjacent to the neighborhood were also completely demolished. [1] Grassy fields in this area also sustained extreme ground scouring of up to 18 inches (46 cm). [5] As a result of this, the path was heavily studied due to its visibility and ground scarring. [5] In total, the tornado dealt $10–20 million (1997 USD) in damage to Double Creek Estates. [1]
After exiting the Double Creek Estates area, the tornado then crossed over a county road while paralleling Spears Ranch Road. [14] After continuing into a cedar tree forest, it began to rapidly weaken, crossing over Appaloosa Cove Road before dissipating. [5] The National Centers for Environmental Information (NCEI) concluded that it had lifted at 3:53 pm, remaining on the ground for 13 minutes and traversing 5.1 miles (8.2 km). [5] [8]
The Jarrell tornado was the subject of a well-known photograph, now known as the "Dead Man Walking". [15] It was taken by Scott Beckwith, and the picture became known for its resemblance to the grim reaper, a figure that commonly represents death in several cultures. [16]
The image consists of the tornado, shrouded in debris, with the main vortex and an adjacent subvortex making "leg" shapes near the bottom of the tornado, giving it the appearance of a giant silhouette walking across the ground. A third subvortex separate from the main funnel is also seen. [16] The image, which is just one in a sequence of 8 photographs taken as the tornado grew in size, has been widely called an example of pareidolia. [16] The photo has received international attention and the Jarrell tornado has popularized the "Dead Man Walking" nickname for similar multi-vortex tornadoes with "legs". [15]
The tornado overall caused widespread damage to structures, and destroyed an estimated 40 family residences. [17] Of these estimated 40 homes, multiple were completely swept off their foundations as a result of the wind. [18] Many of the structures that were swept away were located in the double Creek Estates. The damage from the tornado was classified as F5 severity throughout most of the tornado's path. [19] Approximately $40 million in damage was inflicted upon property with another $100,000 (1997 USD) inflicted upon crops. [1] Additionally, the tornado picked up cars which were either mangled beyond recognition or torn apart. At least six recognizable cars were found over 300 yards (270 m) away, despite being crushed and mud-covered. Many were never recovered, and are presumed to have been "ground up" inside the debris ball. All trees in the subdivision were completely debarked, with one small tree documented to have had an electrical cord pierced through its trunk. [1]
Out of the 131 residents who lived in or near Double Creek Estates, 31 were initially believed to have been killed, but that number was lowered to 27. [19] [20] The remains of these people were found at over 30 locations, and the majority of the deaths were reported in the Morbidity and Mortality Weekly Report as being caused by bodily and head trauma and one fatality was reported to have been caused by asphyxia. Bodily remains were later found at 30 locations, and the physical trauma inflicted on some of the tornado victims was so extreme that first responders reportedly had difficulty distinguishing human remains from the remains of animals at the sites, as the remains were reportedly "ground up" in the winds of the tornado. [21] The sheer strength and intensity of the tornado, as it was in Jarrell, gave the people in its direct path little time to get to safety. Most of the homes that were located in Double Creek Estates at the time were constructed on a slab foundation and lacked of a basement. Up to nineteen people had sought refuge in a single storm cellar. [22] Many residents of the Double Creek Estates had followed the recommended safety procedures, but were still killed because of the strength of the tornado. [23] Some people had chosen to evacuate ahead of the tornado, which may have saved lives. Despite the near-complete destruction of houses on the edge of the tornado, some walls were left standing, protecting several residents. [1] One survivor holed up in a bathtub and was flung several hundred feet from her house onto a road. [23]
Three entire families were killed in the Double Creek Estates area: the Igo family (five members), the Smith family (three members) and the Moehring family (four members). [21] An additional thirteen people were reportedly transported to a hospital after the event; Most of the wounded had abrasions and lacerations due to debris from the tornado. [24] Nine families in Jarrell had more than one member die in the tornado, and the youngest victim was five years old. [1]
Around 300 cattle grazing in a nearby pasture were killed and some were found 0.25 miles (400 m) away. Hundreds of these bodies, including domesticated animals were found dismembered, lacking limbs, decapitated or skinned. [5] [1]
Within minutes after the tornado's impact, emergency management, police, and other volunteers began search-and-rescue operations in Jarrell. Numerous different agencies assisted in the search-and-rescue process, including the Texas Department of Public Safety Police, Texas National Guard, and other smaller agencies. Relief operations, which covered 211 homes and persons damaged or wounded in the tornado, cost an estimated $250,000 (1997 USD); community donations covered at least $200,000 (1997 USD) of the expenses. [25] The tornado knocked out power in Jarrell, effectively stunting communications between emergency services and residents. Cell phones were not functional, and families of affected residents became increasingly concerned due to an inability to communicate. [26] During the emergency response to the affected areas, emergency services almost drove past Double Creek Estates, unaware that houses had stood there. The Double Creek Estates subdivision quickly became the focal point of search-and-rescue and recovery efforts, which were aided by civilians and volunteer workers. [26]
The Jarrell Volunteer Fire Department organized a temporary morgue. Although a death toll of 30 people was initially reported, that figure was later revised to a final tally of 27. [25] A memorial park, which includes twenty-seven trees to commemorate the victims, was built in the Double Creek Estates area. Many impacted people in Double Creek Estates remained in the general area amid recovery efforts stemming from the tornado. [27]
Then-governor of Texas George W. Bush [28] declared Williamson County a disaster area, later stating during a visit to Jarrell on May 28 that it was "the worst tornado I've ever seen". [27] U.S. Senator Kay Bailey Hutchison also visited Jarrell and Cedar Park. Bush later requested federal aid for Williamson and Bell counties with support from Hutchinson. [27] The Federal Emergency Management Agency elected not to provide federal aid, citing the contributions from private and state sources. Instead, the Small Business Administration and U.S. Department of Agriculture made available loans for the rebuilding of homes, farms, and ranches. [27] Between May 29 and June 1, the Office of the Federal Coordinator for Meteorological Services and Supporting Research carried out aerial and ground surveys of the tornadic damage in Texas in coordination with the Texas Wing Civil Air Patrol. [29]
In the six days following the event, the Office of the Federal Coordinator for Meteorological Services and Supporting Research conducted multiple surveys from the air and on the ground to survey the track of the tornado and the damage caused by it. In coordination from the Civil Air Patrol in the state, the tornado received an F5 rating. [8]
There have been multiple in-depth case studies conducted on the tornado since May 1997, most of which covered the impacts to structures and victims as well as the conditions that produced it. [13] [30] [24]
A case study and critique was published by the National Institute of Standards and Technology, which covered the structural damage caused by the tornado and the track that it left. The NIST also published a detailed critique of the Fujita Scale as a direct result of the Jarrell tornado, which was at the time rated an F5. [13] The critique claimed that the Fujita scale failed to account for critical pointers in the assessment of the Jarrell tornado for two engineering factors: the structural construction quality and the specific winds speeds at the specific locations that were surveyed by the National Weather Service. [13] The case study concluded that some of the homes at Double Creek Estates did have small structural integrity issues, which includes factors such as a lack of sufficient anchor bolts and steel straps in the house foundations. However, despite the findings by the study, the tornado's rating remained as an F5. [8]
The University of Wisconsin-Madison also published a case study on the event, authored by Andrew Mankowski, which detailed the weather conditions that caused the tornado to form and how it became as violent as it was. [30] The study said that several meteorological conditions were responsible for the tornado being produced, due in part of a cold front, frontogenesis, and a very unstable warm air mass that had convective available potential energy (CAPE) values topping 6000 j/kg. [30] The latter factor, according to Mankowski, contributed to directional shear which formed the supercells. This caused the violent rotation that eventually produced the Jarrell tornado, and the subsequent strength of it. [30]
The Centers for Disease Control and Prevention (CDC), a U.S. government-affiliated disease control group, produced a study on the casualties of the tornado, including in-depth explanations of the injuries sustained to the bodies of victims and lengths of hospital stays of them. [24] The study and survey concluded that thirty-three people were transported to area hospitals with various injuries, with the most common ones lacerations, contusions, and abrasions. [24] It also noted the lack of shelters that had caused some of the fatalities, and recommended that more storm shelters be installed in Jarrell. [24]
Numerous other groups and organizations conducted small case studies and surveys in the wake of the tornado, including the Federal Emergency Management Agency (FEMA) [31] and the Regional and Mesocale Meteorology Branch (RaMMB). [32] The American Meteorological Society (AMS) also conducted a case study on the event, discussing the meteorological conditions that caused the event and the significance of the Jarrell tornado. [31] A small case study by the NOAA had concluded that the Emergency Alert System (EAS) was not activated in a timely manner to warn about the tornado. [1] Many warning systems had also failed, and the study recommended that emergency alerts and tornado warnings be issued earlier. [1]
A tornado is a violently rotating column of air that is in contact with both the surface of the Earth and a cumulonimbus cloud or, in rare cases, the base of a cumulus cloud. It is often referred to as a twister, whirlwind or cyclone, although the word cyclone is used in meteorology to name a weather system with a low-pressure area in the center around which, from an observer looking down toward the surface of the Earth, winds blow counterclockwise in the Northern Hemisphere and clockwise in the Southern. Tornadoes come in many shapes and sizes, and they are often visible in the form of a condensation funnel originating from the base of a cumulonimbus cloud, with a cloud of rotating debris and dust beneath it. Most tornadoes have wind speeds less than 180 kilometers per hour, are about 80 meters across, and travel several kilometers before dissipating. The most extreme tornadoes can attain wind speeds of more than 480 kilometers per hour (300 mph), can be more than 3 kilometers (2 mi) in diameter, and can stay on the ground for more than 100 km (62 mi).
A supercell is a thunderstorm characterized by the presence of a mesocyclone, a deep, persistently rotating updraft. Due to this, these storms are sometimes referred to as rotating thunderstorms. Of the four classifications of thunderstorms, supercells are the overall least common and have the potential to be the most severe. Supercells are often isolated from other thunderstorms, and can dominate the local weather up to 32 kilometres (20 mi) away. They tend to last 2–4 hours.
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. For these reasons, the outbreak is known in Oklahoma as the May 3rd outbreak or the Oklahoma tornado outbreak of 1999.
A deadly tornado outbreak occurred in Central Texas during the afternoon and evening of May 27, 1997, in conjunction with a southwestward-moving cluster of supercell thunderstorms. These storms produced 20 tornadoes, mainly along the Interstate 35 corridor from northeast of Waco to north of San Antonio. The strongest tornado was an F5 tornado that leveled parts of Jarrell, killing 27 people and injuring 12 others. Overall, 30 people were killed and 33 others were hospitalized by the severe weather.
Jarrell is a city in Williamson County, Texas, United States. The total population is 1,753 according to the 2020 census.
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 on the Fujita Scale, holds records for longest path length at 219 miles (352 km) and longest duration at about 3+1⁄2 hours. The 1974 Guin tornado had the highest forward speed ever recorded in a violent tornado, at 75 mph (121 km/h). The deadliest tornado in world history was the Daulatpur–Saturia tornado in Bangladesh on April 26, 1989, which killed approximately 1,300 people. In the history of Bangladesh, at least 19 tornadoes killed more than 100 people each, almost half of the total for the world. The most extensive tornado outbreak on record was the 2011 Super Outbreak, which resulted in 367 tornadoes and 324 tornadic fatalities, whereas the 1974 Super Outbreak was the most intense tornado outbreak on tornado expert Thomas P. Grazulis's outbreak intensity score with 578, as opposed to the 2011 outbreak's 378.
A deadly series of at least 33 tornadoes hit at least 10 different U.S. states on May 9–11, 1953. Tornadoes appeared daily from Minnesota in the north to Texas in the south. The strongest and deadliest tornado was a powerful F5 tornado that struck Waco, Texas on May 11, causing 114 of the 144 deaths in the outbreak. Alongside the 1902 Goliad tornado, it was the deadliest tornado in Texas history and is the 11th deadliest tornado in U.S. history. The tornado's winds demolished more than 600 houses, 1,000 other structures, and over 2,000 vehicles. 597 injuries occurred, and many survivors had to wait more than 14 hours for rescue. The destruction dispelled a myth that the geography of the region spared Waco from tornadoes, and along with other deadly tornadoes in 1953, the Waco disaster was a catalyst for advances in understanding the link between tornadoes and radar-detected hook echoes. It also generated support for improved civil defense systems, the formation of weather radar networks, and improved communications between stakeholders such as meteorologists, local officials, and the public.
Tornado myths are incorrect beliefs about tornadoes, which can be attributed to many factors, including stories and news reports told by people unfamiliar with tornadoes, sensationalism by news media, and the presentation of incorrect information in popular entertainment. Common myths cover various aspects of the tornado, and include ideas about tornado safety, the minimization of tornado damage, and false assumptions about the size, shape, power, and path of the tornado itself.
The Enhanced Fujita scale rates tornado intensity based on the severity of the damage they cause. It is used in some countries, including the United States and France. The EF scale is also unofficially used in other countries, including China.
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.
The 2007 Elie tornado was a small but extremely powerful and erratic tornado that occurred during the evening of June 22, 2007. The powerful F5 tornado that struck the town of Elie, in the Canadian province of Manitoba was known for its unusual path, how it was during its path, a rope to cone and how it is unique compared to other F5/EF5 tornadoes. It was part of a small two-day tornado outbreak that occurred in the area and reached a maximum width of 150 yards (140 m). The tornado was unusual because it caused the extreme damage during its roping out stage at a mere 35 yards (32 m) in width and moved extremely slowly and unpredictably. The tornado tracked primarily southeast, as opposed to the usual northeast, and made multiple loops and sharp turns. Because Environment Canada adopted the Enhanced Fujita scale in 2013, there will be no more tornadoes with an F5 rating, making this tornado the first confirmed F5 tornado in Canada and the last F5 tornado in the world.
On on June 7–8, 1984, a significant severe weather and tornado event took place across the central United States from North Dakota to Kansas. The tornado outbreak produced several significant tornadoes including an F5 tornado which traveled through Barneveld, Wisconsin, in the early hours of June 8. 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.
Tornadoes are more common in the United States than in any other country or state. The United States receives more than 1,200 tornadoes annually—four times the amount seen in Europe. Violent tornadoes—those rated EF4 or EF5 on the Enhanced Fujita Scale—occur more often in the United States than in any other country.
This page documents the tornadoes and tornado outbreaks of 1997, primarily in the United States. Most tornadoes form in the U.S., although some events may take place internationally. Tornado statistics for older years like this often appear significantly lower than modern years due to fewer reports or confirmed tornadoes, however by the 1990s tornado statistics were coming closer to the numbers we see today.
This page documents the tornadoes and tornado outbreaks of 1998, primarily in the United States. Most tornadoes form in the U.S., although some events may take place internationally. Tornado statistics for older years like this often appear significantly lower than modern years due to fewer reports or confirmed tornadoes, however by the 1990s tornado statistics were coming closer to the numbers we see today.
The 1999 Bridge Creek–Moore tornado was a large, long-lived and exceptionally powerful F5 tornado in which the highest wind speed 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 Oklahoma City 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.
The following is a glossary of tornado terms. It includes scientific as well as selected informal terminology.
The 2011 Philadelphia, Mississippi Tornado was an extremely powerful and fast-moving multi-vortex tornado that touched down in eastern Mississippi on the afternoon of April 27, 2011. Part of the historic 2011 Super Outbreak, the largest tornado outbreak on record, this was the first of four EF5 tornadoes to touch down that day and the first such storm in Mississippi since the 1966 Candlestick Park tornado. While on the ground for 30 minutes, it traveled along a 28.28-mile (45.51 km) path through four counties, leaving behind three deaths, eight injuries, and $1.1 million in damage.