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    Radar Observations of Ice Spheres in Free Fall

    Source: Journal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 001::page 103
    Author:
    Willis, J. T.
    ,
    Browning, K. A.
    ,
    Atlas, D.
    DOI: 10.1175/1520-0469(1964)021<0103:ROOISI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Simultaneous measurements of the radar cross section and fallspeed of 5 cm (and larger) ice spheres falling in free air have been obtained using a high-precision tracking radar operating at a wavelength of 5.47 cm. While they were dry, the spheres fell with supercritical Reynolds numbers and drag coefficients of only 0.24 to 0.30. These coefficients are much smaller than those normally attributed to hailstones under any conditions. The surface of one sphere, 5.1 cm in diameter, became wet during its fall. This was accompanied by a 5 db decrease in its normalized radar cross section and a twofold increase in its drag coefficient. The implications of these observations are discussed.
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      Radar Observations of Ice Spheres in Free Fall

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150603
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    contributor authorWillis, J. T.
    contributor authorBrowning, K. A.
    contributor authorAtlas, D.
    date accessioned2017-06-09T14:13:16Z
    date available2017-06-09T14:13:16Z
    date copyright1964/01/01
    date issued1964
    identifier issn0022-4928
    identifier otherams-14982.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150603
    description abstractSimultaneous measurements of the radar cross section and fallspeed of 5 cm (and larger) ice spheres falling in free air have been obtained using a high-precision tracking radar operating at a wavelength of 5.47 cm. While they were dry, the spheres fell with supercritical Reynolds numbers and drag coefficients of only 0.24 to 0.30. These coefficients are much smaller than those normally attributed to hailstones under any conditions. The surface of one sphere, 5.1 cm in diameter, became wet during its fall. This was accompanied by a 5 db decrease in its normalized radar cross section and a twofold increase in its drag coefficient. The implications of these observations are discussed.
    publisherAmerican Meteorological Society
    titleRadar Observations of Ice Spheres in Free Fall
    typeJournal Paper
    journal volume21
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1964)021<0103:ROOISI>2.0.CO;2
    journal fristpage103
    journal lastpage108
    treeJournal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian