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    Solid Water-Insoluble Particles in Hailstones and Their Geophysical Significance

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 004::page 481
    Author:
    Rosinski, J.
    DOI: 10.1175/1520-0450(1966)005<0481:SWIPIH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: By melting concentric layers of ice, the size distribution and concentration of solid water-insoluble particles accumulated in hailstones were determined for three hailstorms in Colorado. It was found that in approximately 50 per cent of the hailstones analyzed, particle concentration in ice increased with radial distance. Following an equation derived for this category of hailstones, a relationship is shown among liquid water content of a cloud, concentration of solid particles in cloud droplets, speed of the hailstone, and its residence time in the atmosphere. Spatial distribution of solid particles in hailstones was also determined by slicing hailstones and subsequently separating particles from the ice by sublimation under low pressure. It was found that some of the hailstones analyzed were oriented during their growth.
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      Solid Water-Insoluble Particles in Hailstones and Their Geophysical Significance

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4215745
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    contributor authorRosinski, J.
    date accessioned2017-06-09T16:45:38Z
    date available2017-06-09T16:45:38Z
    date copyright1966/08/01
    date issued1966
    identifier issn0021-8952
    identifier otherams-7361.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215745
    description abstractBy melting concentric layers of ice, the size distribution and concentration of solid water-insoluble particles accumulated in hailstones were determined for three hailstorms in Colorado. It was found that in approximately 50 per cent of the hailstones analyzed, particle concentration in ice increased with radial distance. Following an equation derived for this category of hailstones, a relationship is shown among liquid water content of a cloud, concentration of solid particles in cloud droplets, speed of the hailstone, and its residence time in the atmosphere. Spatial distribution of solid particles in hailstones was also determined by slicing hailstones and subsequently separating particles from the ice by sublimation under low pressure. It was found that some of the hailstones analyzed were oriented during their growth.
    publisherAmerican Meteorological Society
    titleSolid Water-Insoluble Particles in Hailstones and Their Geophysical Significance
    typeJournal Paper
    journal volume5
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1966)005<0481:SWIPIH>2.0.CO;2
    journal fristpage481
    journal lastpage492
    treeJournal of Applied Meteorology:;1966:;volume( 005 ):;issue: 004
    contenttypeFulltext
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