The history of tornado research spans back centuries, with the earliest documented tornado occurring in 200 CE and academic studies on them starting in the 18th century. Several people throughout history are known to have researched tornadoes. This is a timeline of government or academic research into tornadoes.
Early studies The earliest-known tornado occurred in Sardegna, Sardinia and Corsica, Roman Empire (modern-day Italy) in 200. The earliest-known German tornado struck Freising (modern day Germany) in 788. The earliest-known Irish tornado appeared on April 30, 1054, in Rostella, near Kilbeggan. The earliest-known British tornado hit central London on October 23, 1091, and was especially destructive, with modern research classifying it as an F4 on the Fujita scale. After the discovery of the New World, tornado documentation expanded into the Americas. On August 21, 1521, an apparent tornado is recorded to have struck Tlatelolco (present day Mexico City), just two days before the Aztec capital's fall to Cortés. Many other tornadoes are documented historically within the Basin of Mexico. The first confirmed tornado in the United States struck Rehoboth, Massachusetts, in August 1671. The first confirmed tornadic death in the United States occurred on July 8, 1680, after a tornado struck Cambridge, Massachusetts.
First tornadic case study
The first case study on a tornado took place following the violent 1764 Woldegk tornado, which struck around Woldegk, Duchy of Mecklenburg-Strelitz, Holy Roman Empire (modern-day Germany). Between 1764 and 1765, German scientist Gottlob Burchard Genzmer published a detailed survey of the damage path from the tornado. It covers the entire, 33km (18.6mi) long track and also includes eyewitness reports as well as an analysis of the debris and hail fallout areas. Genzmer calls the event an "Orcan" and only compares it to waterspouts or dust devils. Based on the damage survey, modern day meteorologists from the ESSL were able to assign a rating of F5, on the Fujita scale, and T11 on the TORRO scale, making it the earliest known F5 tornado worldwide. The T11 rating on the TORRO scale also places this event among the most violent tornadoes ever documented worldwide.
First studies by country In May 1820, Józef Karol Skrodzki, Professor at the University of Warsaw, read a paper describing a tornado that occurred in Mazew, Łęczyca County in Poland on August 10, 1819. It was described that the tornado had the appearance of a funnel whose color seemed different depending on the lighting, and that it damaged several buildings by tearing off roofs, damaging the structure, and lifting a hay wagon into the air. The paper was published in a collection of works by the Warsaw Society of Friends of Learning in 1821.
In 1838, the earliest recorded Asian tornado struck near the city of Calcutta in present-day West Bengal, India. It was described as moving remarkably slow across its 16-mile (26 km) path southeast over the span of 2 to 3 hours. It was recorded to cause significant damage to the area, including 3.5-pound (1.6 kg) hail being observed at the Dum Dum weather observatory. Between 1839 and 1841, a detailed survey of damage path of significant tornado that struck New Brunswick, New Jersey, on June 19, 1835, which was the deadliest tornado in New Jersey history, occurred. The path was surveyed by many scientists on account of its location between New York City and Philadelphia, including early tornado theorists James Pollard Espy and William Charles Redfield. Scientists disagreed whether there was whirling, convergent, or rotational motion. A conclusion that remains accurate today is that the most intense damage tends to be on right side of a tornado (with respect to direction of forward movement), which was found to be generally easterly. In 1840, the earliest known intensive study of a tornadic event published in Europe, by French scientist Athanase Peltier. In 1865, the first in India and earliest known scientific survey of a tornado that analyzed structure and dynamics was published by Indian scientist Chunder Sikur Chatterjee. The path damage survey of a tornado that occurred at Pundooah (now Pandua), Hugli district, West Bengal, India, was documented on maps and revealed multiple vortices, the tornadocyclone, and direction of rotation, predating work by John Park Finley, Alfred Wegener, Johannes Letzmann, and Ted Fujita.
Research by topic
Tornadogenesis
In December 1898, Dr. B. F. Duke, along with Dr. Cleveland Abbe, published a paper regarding the United States's Weather Bureau's first official theory on how tornadoes form after Duke observed the formation of a tornado near Pascagoula, Mississippi, in April 1894. This theory included that winds have to be moving in two different directions ("northerly and southerly") and that when those winds meet, they form a rapid updraft, which forms a very buoyant cloud. The buoyant cloud then will "suck up the air beneath it with such violence as to form a waterspout over the ocean or a tornado over the land and the winds immediately below it are suddenly and greatly increased". Dr. Abe then theorized that "it is possible that we may have violent whirls with horizontal axes", for the first theory of horizontal vortices within tornadoes. In 1960, Bernard Vonnegut suggested that electricity in thunderstorms may power tornadoes.
Characteristics of tornadoes
In April 1899, Dr. Cleveland Abbe, along with Professor A. W. Baker and E. L. Dinniston, published an article regarding the characteristics of tornadoes. In the study and analysis, Abbe discovered that tornadoes in the United States rotate counterclockwise, just the same as a large low-pressure system. Abbe also stated that this rotation rule for tornadoes "is almost invariable". In November 1900, S. C. Emery with the United States Weather Bureau conducted a case study, including detailed damage surveys, for a small tornado outbreak in Tennessee, Mississippi and Arkansas on November 19, 1900. In the study, Emery surveyed and mapped that one of the tornadoes "divided" into two nearly parallel parts, or that it had a "zig zag" motion, as some buildings were not damaged and others destroyed. Emery also stated he was "inclined to believe the latter explanation as more reasonable". Emery also noted one of the tornadoes had an average forward speed of 60 mph (97 km/h) and that a separate tornado travelled 215 miles (346 km).
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