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    Hail and Raindrop Size Distributions from a Swiss Multicell Storm

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 001::page 91
    Author:
    Federer, B.
    ,
    Waldvogel, A.
    DOI: 10.1175/1520-0450(1975)014<0091:HARSDF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Time-resolved hail and raindrop size distributions measured simultaneously during a multicellular hailstorm are presented. The time variation of the size distributions allowed a detailed analysis of the structure of the hailswath. It consisted of four hail cells with a duration of 2?3 min each. The number density of the hailstones increased and the mean diameter decreased during the lifetime of a cell. The contributions of liquid water and ice water content to the total water W were about equal; W was never larger than 5 g m?3. The size distributions were well approximated by an exponential law. The mean distribution is given by NH (D) = 12 exp (?0.42D). The distributions are compared with measurements and calculations of other authors and the differences are discussed.
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      Hail and Raindrop Size Distributions from a Swiss Multicell Storm

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232089
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    contributor authorFederer, B.
    contributor authorWaldvogel, A.
    date accessioned2017-06-09T17:37:42Z
    date available2017-06-09T17:37:42Z
    date copyright1975/02/01
    date issued1975
    identifier issn0021-8952
    identifier otherams-8832.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232089
    description abstractTime-resolved hail and raindrop size distributions measured simultaneously during a multicellular hailstorm are presented. The time variation of the size distributions allowed a detailed analysis of the structure of the hailswath. It consisted of four hail cells with a duration of 2?3 min each. The number density of the hailstones increased and the mean diameter decreased during the lifetime of a cell. The contributions of liquid water and ice water content to the total water W were about equal; W was never larger than 5 g m?3. The size distributions were well approximated by an exponential law. The mean distribution is given by NH (D) = 12 exp (?0.42D). The distributions are compared with measurements and calculations of other authors and the differences are discussed.
    publisherAmerican Meteorological Society
    titleHail and Raindrop Size Distributions from a Swiss Multicell Storm
    typeJournal Paper
    journal volume14
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1975)014<0091:HARSDF>2.0.CO;2
    journal fristpage91
    journal lastpage97
    treeJournal of Applied Meteorology:;1975:;volume( 014 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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