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    Further Studies of Large, Water-Insoluble Particles within Hailstones

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 005::page 882
    Author:
    Rosinski, Jan
    ,
    Knight, Charles A.
    ,
    Nagamoto, Clarence T.
    ,
    Morgan, Griffith M.
    ,
    Knight, Nancy C.
    ,
    Prodi, Franco
    DOI: 10.1175/1520-0469(1979)036<0882:FSOLWI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Results of a previous study have been confirmed by additional measurements on many hailstones from several different areas. They indicate that relatively clear hailstone embryos, interpreted as frozen drops, are associated with large soil or organic particles. Opaque (bubbly) embryos do not contain foreign particles larger than 40 ?m diameter. The difference is observed even when the two hailstone embryo types occur in a single hailfall. The results suggest that different embryo types originate in different parts of a storm and are carried by the thunderstorm airflow into a common final growth and fallout region.
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      Further Studies of Large, Water-Insoluble Particles within Hailstones

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4153626
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    • Journal of the Atmospheric Sciences

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    contributor authorRosinski, Jan
    contributor authorKnight, Charles A.
    contributor authorNagamoto, Clarence T.
    contributor authorMorgan, Griffith M.
    contributor authorKnight, Nancy C.
    contributor authorProdi, Franco
    date accessioned2017-06-09T14:20:48Z
    date available2017-06-09T14:20:48Z
    date copyright1979/05/01
    date issued1979
    identifier issn0022-4928
    identifier otherams-17702.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153626
    description abstractResults of a previous study have been confirmed by additional measurements on many hailstones from several different areas. They indicate that relatively clear hailstone embryos, interpreted as frozen drops, are associated with large soil or organic particles. Opaque (bubbly) embryos do not contain foreign particles larger than 40 ?m diameter. The difference is observed even when the two hailstone embryo types occur in a single hailfall. The results suggest that different embryo types originate in different parts of a storm and are carried by the thunderstorm airflow into a common final growth and fallout region.
    publisherAmerican Meteorological Society
    titleFurther Studies of Large, Water-Insoluble Particles within Hailstones
    typeJournal Paper
    journal volume36
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1979)036<0882:FSOLWI>2.0.CO;2
    journal fristpage882
    journal lastpage891
    treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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