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    Photogrammetric Velocities for the Great Bend, Kansas, Tornado of 30 August 1974: Accelerations and Asymmetries

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 004::page 485
    Author:
    Golden, J. H.
    ,
    Purcell, D.
    DOI: 10.1175/1520-0493(1977)105<0485:PVFTGB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Late in the afternoon of 30 August 1974 a dozen tornadoes were observed over open farming terrain within a 65 km radius of Great Bend, Kans. All but one of the tornadoes traveled mainly toward the southeast; the other tornado moved northeastward and produced damage near Galatia. One of the largest tornadoes occurred about 40 km west?southwest of Great Bend, and high-resolution motion picture films were taken by a news photographer 2.7 km north of the vortex. The vortex was visible as a rotating column of dense dust and small debris particles. Photogrammetric analysis and tracking of debris in the rotating dust column yield velocities as high as 85 m s?1. Maximum measured horizontal wind speeds are 75 m s?1at z≈90 m AGL and maximum rising motions are 60 m s?1at z≈80 m A remarkable dark band of dust, about 35 m high, apparently outlined a major inflow jet of air accelerating into the vortex at low levels from the west-southwest. The dust band has appeared in other tornado photograph (e.g., Kessler, 1972) but its possible importance to the overall flow structure fuss not been emphasized.
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      Photogrammetric Velocities for the Great Bend, Kansas, Tornado of 30 August 1974: Accelerations and Asymmetries

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4199618
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    • Monthly Weather Review

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    contributor authorGolden, J. H.
    contributor authorPurcell, D.
    date accessioned2017-06-09T16:01:34Z
    date available2017-06-09T16:01:34Z
    date copyright1977/04/01
    date issued1977
    identifier issn0027-0644
    identifier otherams-59098.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199618
    description abstractLate in the afternoon of 30 August 1974 a dozen tornadoes were observed over open farming terrain within a 65 km radius of Great Bend, Kans. All but one of the tornadoes traveled mainly toward the southeast; the other tornado moved northeastward and produced damage near Galatia. One of the largest tornadoes occurred about 40 km west?southwest of Great Bend, and high-resolution motion picture films were taken by a news photographer 2.7 km north of the vortex. The vortex was visible as a rotating column of dense dust and small debris particles. Photogrammetric analysis and tracking of debris in the rotating dust column yield velocities as high as 85 m s?1. Maximum measured horizontal wind speeds are 75 m s?1at z≈90 m AGL and maximum rising motions are 60 m s?1at z≈80 m A remarkable dark band of dust, about 35 m high, apparently outlined a major inflow jet of air accelerating into the vortex at low levels from the west-southwest. The dust band has appeared in other tornado photograph (e.g., Kessler, 1972) but its possible importance to the overall flow structure fuss not been emphasized.
    publisherAmerican Meteorological Society
    titlePhotogrammetric Velocities for the Great Bend, Kansas, Tornado of 30 August 1974: Accelerations and Asymmetries
    typeJournal Paper
    journal volume105
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1977)105<0485:PVFTGB>2.0.CO;2
    journal fristpage485
    journal lastpage492
    treeMonthly Weather Review:;1977:;volume( 105 ):;issue: 004
    contenttypeFulltext
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