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Tornado outbreak sequence of May 1896

Extremely devastating windstorm in the United States From Wikipedia, the free encyclopedia

Tornado outbreak sequence of May 1896
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From May 24–28, 1896, a violent tornado outbreak sequence—considered one of the worst on record—struck much of the United States, killing at least 388 people and injuring 1,490 or more. At least 26 tornadoes occurred, including intense, long-lived families. Retroactively rated F5 on the Fujita scale, the strongest tornado of the outbreak struck Michigan, killing 47 or more people. F4 tornadoes in three other states collectively caused most of the remaining deaths, among them a potent twister that impacted Greater St. Louis, claiming 255 lives and becoming the third-deadliest U.S. tornado on record. Additionally, at least one tornado crossed into Canada, inflicting more damage there. Tornado expert Thomas P. Grazulis dubbed the severe weather episode "perhaps the most violent single week of tornado activity in United States history".[1][note 2]

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Confirmed tornadoes

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Prior to 1990, there is a likely undercount of tornadoes, particularly E/F0–1, with reports of weaker tornadoes becoming more common as population increased. A sharp increase in the annual average E/F0–1 count by approximately 200 tornadoes was noted upon the implementation of NEXRAD Doppler weather radar in 1990–1991.[4][note 3] 1974 marked the first year where significant tornado (E/F2+) counts became homogenous with contemporary values, attributed to the consistent implementation of Fujita scale assessments.[8][note 4] Numerous discrepancies on the details of tornadoes in this outbreak exist between sources. The total count of tornadoes and ratings differs from various agencies accordingly. The list below documents information from the most contemporary official sources alongside assessments from tornado historian Thomas P. Grazulis.

May 24 event

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May 25 event

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May 27 event

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May 28 event

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Whigville–Ortonville–Oakwood–Thomas, Michigan

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Late in the evening of May 25, an extremely intense tornado touched down in eastern Michigan and moved northeast. It affected portions of Oakland and Lapeer counties northwest of Detroit. Communities affected included Whigville, Ortonville, Oakwood, and Thomas. Farms and homes were leveled or swept away, with whole families being killed. Debris was carried 12 mi (19 km) away, and trees were debarked, with even small twigs stripped bare in some cases, as if by "an experienced artisan". Fragments of a home in Thomas were dispersed up to 10 mi (16 km) away. A piano from that residence was found 200 yd (180 m) away from the foundation, with one end "pounded full of grass". Damage surveyors reported that grass in the center of the circulation was "pounded down into the earth, as if it had been washed into the earth by a heavy flow of water". 22 or more people were killed in Ortonville, 10 in Oakwood, three in Thomas, four north of Oxford, and three in Whigville, along with others in rural areas. Nine of the dead were in a home at Ortonville. Up to seven communities reported deaths. At least 100 people were injured. With 47 deaths, this is the second-deadliest tornado ever in Michigan, trailing only the Flint–Beecher F5 of 1953, which killed 116 in Genesee County just outside Flint.[29]

St. Louis, Missouri/East St. Louis, Illinois

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The third deadliest tornado in United States history struck the Greater St. Louis area in both Missouri and Illinois, killing 255 people, injuring at least 1,000 more, and causing more than $10 million in damages. It formed just northwest of Tower Grove Park in St. Louis, attended by strong downbursts. At least 137 people died as the tornado traversed the core of the downtown area, leaving a continuous, 1-mile-wide (1.6 km) swath of destroyed homes, schools, saloons, factories, mills, churches, parks, and railroad yards in its wake. Some of destroyed homes were all but completely swept away, but damage to trees and roofs in most areas was less severe. Numerous trees were downed at the 36-acre (0.15 km2) Lafayette Park, and a barometer recorded a drop to 26.74 inHg (906 mb) at this location.

After devastating the city of St. Louis, the tornado crossed the Mississippi River and struck the Eads Bridge, where a 2 in × 10 in (51 mm × 254 mm) wooden plank was found driven through a 516 in (7.9 mm) wrought iron plate. Uncounted others may have died on boats on the river, which could have swept their bodies downriver where they could not be recorded in the official death toll. The tornado continued into East St. Louis, Illinois, where its path was narrower, but its strength became even more intense. Homes and buildings along the river were completely swept away and a quarter of the buildings there were damaged or destroyed, though many of the structures were frail. An additional 118 people were killed, 35 of whom were at the Vandalia railroad freight yards.[30]

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Notes

  1. All losses are in 1896 United States dollars unless otherwise noted.
  2. An outbreak is generally defined as a group of at least six tornadoes (the number sometimes varies slightly according to local climatology) with no more than a six-hour gap between individual tornadoes. An outbreak sequence, prior to (after) the start of modern records in 1950, is defined as a period of no more than two (one) consecutive days without at least one significant (F2 or stronger) tornado.[2]
  3. Historically, the number of tornadoes globally and in the United States was and is likely underrepresented: research by Grazulis on annual tornado activity suggests that, as of 2001, only 53% of yearly U.S. tornadoes were officially recorded. Documentation of tornadoes outside the United States was historically less exhaustive, owing to the lack of monitors in many nations and, in some cases, to internal political controls on public information.[5] Most countries only recorded tornadoes that produced severe damage or loss of life.[6] Significant low biases in U.S. tornado counts likely occurred through the early 1990s, when advanced NEXRAD was first installed and the National Weather Service began comprehensively verifying tornado occurrences.[7]
  4. The Fujita scale was devised under the aegis of scientist T. Theodore Fujita in the early 1970s. Prior to the advent of the scale in 1971, tornadoes in the United States were officially unrated.[9][10] Tornado ratings were retroactively applied to events prior to the formal adoption of the F-scale by the National Weather Service.[11] While the Fujita scale has been superseded by the Enhanced Fujita scale in the U.S. since February 1, 2007,[12] Canada used the old scale until April 1, 2013;[13] nations elsewhere, like the United Kingdom, apply other classifications such as the TORRO scale.[14]
  5. All dates are based on the local time zone where the tornado touched down; however, all times are in Coordinated Universal Time and dates are split at midnight CST/CDT for consistency.
  6. The listed width values are primarily the average/mean width of the tornadoes, with those having known maximum widths denoted by ♯. From 1952 to 1994, reports largely list mean width whereas contemporary years list maximum width.[15] Values provided by Grazulis are the average width, with estimates being rounded down (i.e. 0.5 mi (0.80 km) is rounded down from 880 yards to 800 yards.[16][17]
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References

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