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    Freezing of Freely Suspended, Supercooled Water Drops in a Large Vertical Wind Tunnel

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 007::page 1101
    Author:
    Spengler, John D.
    ,
    Gokhale, Narayan R.
    DOI: 10.1175/1520-0450(1972)011<1101:FOFSSW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The design and operation of a large vertical wind tunnel (1.8 m diameter updraft) are described, together with the associated special photographic equipment and techniques required for studies of the interactions and freezing of freely suspended water drops. During the first two winters of operation several new and important observations have been made while freezing freely suspended, large supercooled water drops. The terminal velocity of the frozen pellet was found to be very different than that of the liquid drop. If individual drops freeze at ?6C and colder they often exhibit a marked decrease (up to 4 m sec?1) in terminal velocity. Coalescence of a frozen pellet and a liquid drop produces an elongated ice pellet (8?15 mm horizontal axis) with a terminal velocity of 9 m sec?1. When an ice pellet becomes unstable and spins about a horizontal axis, it can obtain a rapid horizontal velocity. Two ice pellets frozen together display the same erratic tumbling. These observations indicate that some ice pellets have greatly increased distances and residence times to grow in the supercooled region of a cloud.
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      Freezing of Freely Suspended, Supercooled Water Drops in a Large Vertical Wind Tunnel

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4227745
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    • Journal of Applied Meteorology

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    contributor authorSpengler, John D.
    contributor authorGokhale, Narayan R.
    date accessioned2017-06-09T17:23:36Z
    date available2017-06-09T17:23:36Z
    date copyright1972/10/01
    date issued1972
    identifier issn0021-8952
    identifier otherams-8441.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227745
    description abstractThe design and operation of a large vertical wind tunnel (1.8 m diameter updraft) are described, together with the associated special photographic equipment and techniques required for studies of the interactions and freezing of freely suspended water drops. During the first two winters of operation several new and important observations have been made while freezing freely suspended, large supercooled water drops. The terminal velocity of the frozen pellet was found to be very different than that of the liquid drop. If individual drops freeze at ?6C and colder they often exhibit a marked decrease (up to 4 m sec?1) in terminal velocity. Coalescence of a frozen pellet and a liquid drop produces an elongated ice pellet (8?15 mm horizontal axis) with a terminal velocity of 9 m sec?1. When an ice pellet becomes unstable and spins about a horizontal axis, it can obtain a rapid horizontal velocity. Two ice pellets frozen together display the same erratic tumbling. These observations indicate that some ice pellets have greatly increased distances and residence times to grow in the supercooled region of a cloud.
    publisherAmerican Meteorological Society
    titleFreezing of Freely Suspended, Supercooled Water Drops in a Large Vertical Wind Tunnel
    typeJournal Paper
    journal volume11
    journal issue7
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1972)011<1101:FOFSSW>2.0.CO;2
    journal fristpage1101
    journal lastpage1107
    treeJournal of Applied Meteorology:;1972:;volume( 011 ):;issue: 007
    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
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