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Debris fallout

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A Correlation coefficient scan reveals a significant volume of lofted debris as high as 30,000 ft (5.7 mi; 9.1 km) during a violent tornado

Debris fallout refers to debris lofted into the air by a tornado that falls back to the ground that can persist well after a tornado has lifted. Debris lofted by stronger tornadoes has been known to travel significant distances, upwards of 200 mi (320 km) on rare occasions. Debris fallout events can be detected on radar using dual polarization products, notably correlation coefficient. Most debris in excess of 1 lb (0.45 kg) is not moved a great distance, however lighter objects, especially paper goods, can be absorbed by the storm's updraft and moved into its forward-flank downdraft where they can be transported further by non-tornadic downdraft winds.[1][2][3]

Mechanism

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The basic mechanism of debris fallout is debris lofted by a tornado's updraft winds high into the atmosphere.[4] Charles E. Anderson completed the first study focusing on debris fallout on the F5 1984 Barneveld tornado, which produced a large survey revealing a trail of paper debris as wide as 23 mi (37 km) at 110 mi (180 km) from Barneveld and a roughly 85 mi (137 km) long path of heavy debris (>1 lb (0.45 kg)).[2] A later study focusing on debris fallout discovered that debris from an intense tornado was lofted as high as 12 km (7.5 mi) into the atmosphere over the 15–20 minutes after the tornado striking a location, before debris was moved further into the tornado's forward-flank downdraft. A photograph had been traced and discovered to have an average speed of 18 m/s (40 mph; 65 km/h) over 30 minutes. [5] A 1993 analysis by Thomas P. Grazulis of 12,651 tornadoes found only 86 had reports of debris being transported over 5 mi (8.0 km) from its origin.[2]

The height of a tornado debris signature is positively and non-linearly correlated with the speed of updraft winds, which is likely compounded by fallout.[6] Debris that falls directly over the vortex can result in an increase in the size of the tornado debris signature on radar.[7]

Examples

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  • 1915 Great Bend tornado – A cancelled check discovered in Palmyra, Nebraska was traced back to Great Bend, Kansas, a distance of 210 mi (340 km) and, at the time, the greatest distance any debris had been lofted by a tornado.[2]
  • 2011 Super Outbreak – A study identified a Facebook page listing over 1700 lost-and-found documents and other light debris from the entire outbreak. Debris was frequently lofted as high as 5.5–6.5 km (3.4–4.0 mi), particularly from the violent (EF4/EF5) tornadoes.[8]
  • 2011 Joplin tornado – A receipt from a tire repair shop dated the same date as the violent EF5 tornado in Joplin, Missouri was discovered several days later in Royal Center, Indiana, 525 mi (845 km) away. This account is disputed as it was revealed family members from Texas stopped in Joplin for repairs, likely forgetting the receipt on a cooler.[9]
  • 2019 Lawrence–Kansas City tornado – A 2020 study focusing on this tornado discovered that lofted debris became visible on radar following the tornado reaching violent intensity. Kansas City International Airport had been under a tornado warning, and 16 minutes after the all-clear was lifted, despite being 75 km (47 mi) from the tornado itself, a ground stop was issued as significant volumes of debris was reported on the runway. An airborne debris signature was evident over the airport up to an hour prior to the first reports of debris.[3]

See also

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References

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  1. ^ Erdman, Jonathan (30 May 2019). "EF4 Kansas Tornado Debris Found 50 Miles Away And That's Not Unusual". The Weather Channel. Retrieved 17 December 2024.
  2. ^ a b c d Snow, John T.; Wyatt, Amy Lee; McCarthy, Ann K.; Bishop, Eric K. (1995). "FALLOUT OF DEBRIS FROM TORNADIC THUNDERSTORMS: An Historical Perspective And Two Examples From VORTEX". American Meteorological Society.
  3. ^ a b Wang, Erik Y.; Bodine, David J.; Kurdzo, James M.; Barham, James; Bowman, Chris; Pietrycha, Pamela. Polarimetric Characteristics of Tornado Debris Fallout During the May 28 2019 Lawrence/Kansas City, KS Tornado (PDF). 100th Annual Meeting Severe Local Storms Symposium.
  4. ^ Dolce, Chris (20 March 2024). "Hook Echo, Debris Ball, Bow Echo: What Meteorologists Mean By These Radar Terms". The Weather Channel. Retrieved 19 December 2024.
  5. ^ Magsig, Michael A.; Snow, John T. (1998). "Long-Distance Debris Transport by Tornadic Thunderstorms.Part I: The 7 May 1995 Supercell Thunderstorm". Monthly Weather Review. 126 (6). American Meteorological Society: 1430. Bibcode:1998MWRv..126.1430M. doi:10.1175/1520-0493(1998)126<1430:LDDTBT>2.0.CO;2.
  6. ^ Cross, Rachael N.; Bodine, David J.; Palmer, Robert D.; Griffin, Casey; Cheong, Boonleng; Torres, Sebastian; Fulton, Caleb; Lujan, Javier; Maruyama, Takashi (1 October 2023). "Exploring Tornadic Debris Signature Hypotheses Using Radar Simulations and Large-Eddy Simulations". Journal of Atmospheric and Oceanic technology. American Meteorological Society.
  7. ^ Van der Broeke, Matthew S. (1 December 2015). "Polarimetric Tornadic Debris Signature Variability and Debris Fallout Signatures". Journal of Applied Meteorology and Climatology.
  8. ^ a b c Knox, John A.; Rackley, Jared A.; Black, Alan W.; Gensini, Vittorio A.; Butler, Michael; Dunn, Corey; Gallo, Taylor; Hunter, Melyssa R.; Lindsey, Lauren; Phan, Minh; Scroggs, Robert; Brustad, Synne (1 September 2013). "Tornado Debris Characteristics And Trajectories During The 27 April 2011 Super Outbreak As Determined Using Social Media Data". Bulletin of the American Meteorological Society. 94 (9). American Meteorological Society: 1371–1380. Bibcode:2013BAMS...94.1371K. doi:10.1175/BAMS-D-12-00036.1.
  9. ^ Koenig, Rob (28 May 2011). "Joplin receipt hitched a ride in a car, not a tornado". St. Louis Public Radio. Retrieved 18 December 2024.