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    Hail Growth Mechanisms in a Colorado Storm. Part I: Dual-Wavelength Radar Observations

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 008::page 1763
    Author:
    Jameson, A. R.
    ,
    Heymsfield, A. J.
    DOI: 10.1175/1520-0469(1980)037<1763:HGMIAC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Extensive comparisons of dual-wavelength (10 and 3 cm) radar data with observations at the ground and penetration aircraft (T-28) measurements of hail in a Colorado storm show that positive hail signals (10 cm reflectivity factor exceeds that at 3 cm) are well correlated with the presence of hail ? 1 cm diameter. Widespread areas of negative hail signals (3 cm reflectivity factor exceeds that at 10 cm) found above the melting level are correlated with the presence of subcentimeter graupel. It is possible, therefore, to discriminate two sizes of particles based on dual-wavelength radar measurements. This finding is exploited in Part II of this work to investigate the evolution of graupel into hail.
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      Hail Growth Mechanisms in a Colorado Storm. Part I: Dual-Wavelength Radar Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153927
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    contributor authorJameson, A. R.
    contributor authorHeymsfield, A. J.
    date accessioned2017-06-09T14:21:41Z
    date available2017-06-09T14:21:41Z
    date copyright1980/08/01
    date issued1980
    identifier issn0022-4928
    identifier otherams-17974.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153927
    description abstractExtensive comparisons of dual-wavelength (10 and 3 cm) radar data with observations at the ground and penetration aircraft (T-28) measurements of hail in a Colorado storm show that positive hail signals (10 cm reflectivity factor exceeds that at 3 cm) are well correlated with the presence of hail ? 1 cm diameter. Widespread areas of negative hail signals (3 cm reflectivity factor exceeds that at 10 cm) found above the melting level are correlated with the presence of subcentimeter graupel. It is possible, therefore, to discriminate two sizes of particles based on dual-wavelength radar measurements. This finding is exploited in Part II of this work to investigate the evolution of graupel into hail.
    publisherAmerican Meteorological Society
    titleHail Growth Mechanisms in a Colorado Storm. Part I: Dual-Wavelength Radar Observations
    typeJournal Paper
    journal volume37
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1980)037<1763:HGMIAC>2.0.CO;2
    journal fristpage1763
    journal lastpage1778
    treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 008
    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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