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    Wind Tunnel Tests of Simulated Spherical Hailstones with Variable Roughness

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 001::page 58
    Author:
    Young, Ronald G. Eng
    ,
    Browning, Keith A.
    DOI: 10.1175/1520-0469(1967)024<0058:WTTOSS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Wind tunnel test data on the relationship between drag coefficient and Reynolds number are presented for solid spherical models with different roughness parameters. Using a wind tunnel with minimal free-stream turbulence it is found that spheres with spherical roughness elements designed to simulate hailstones with rough rime coats exhibit an unexpectedly sharp drop in drag coefficient at critical Reynolds number. For a spherical hailstone with roughness elements as large as 0.02 inch, the transition to the lower drag coefficient could occur when the stone is as small as 1.6 inch in diameter (for a smooth sphere the corresponding transition does not occur unless its diameter exceeds 4 inches).
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      Wind Tunnel Tests of Simulated Spherical Hailstones with Variable Roughness

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150941
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    contributor authorYoung, Ronald G. Eng
    contributor authorBrowning, Keith A.
    date accessioned2017-06-09T14:14:02Z
    date available2017-06-09T14:14:02Z
    date copyright1967/01/01
    date issued1967
    identifier issn0022-4928
    identifier otherams-15286.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150941
    description abstractWind tunnel test data on the relationship between drag coefficient and Reynolds number are presented for solid spherical models with different roughness parameters. Using a wind tunnel with minimal free-stream turbulence it is found that spheres with spherical roughness elements designed to simulate hailstones with rough rime coats exhibit an unexpectedly sharp drop in drag coefficient at critical Reynolds number. For a spherical hailstone with roughness elements as large as 0.02 inch, the transition to the lower drag coefficient could occur when the stone is as small as 1.6 inch in diameter (for a smooth sphere the corresponding transition does not occur unless its diameter exceeds 4 inches).
    publisherAmerican Meteorological Society
    titleWind Tunnel Tests of Simulated Spherical Hailstones with Variable Roughness
    typeJournal Paper
    journal volume24
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1967)024<0058:WTTOSS>2.0.CO;2
    journal fristpage58
    journal lastpage62
    treeJournal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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