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    A Calorimetric Method for Measuring Water Content of Hailstones

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 005::page 715
    Author:
    Gitlin, Sonia N.
    ,
    Fogler, H. Scott
    ,
    Goyer, Guy G.
    DOI: 10.1175/1520-0450(1966)005<0715:ACMFMW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A calorimetric method for measuring the liquid water content of hailstones has been developed. When parameters such as the radiative losses of the system and the changes in heat capacity of the apparatus are eliminated by performing all measurements under identical conditions, the temperature drop is linearly related to the mass of ice melted. For equal masses the temperature drop is smaller if water is present, and there is a linear relationship between the changes in temperature drop and the amount of water present. The water content of hailstones can then be determined from a calibration plot of the changes in temperature drop as a function of the water content of ice.
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      A Calorimetric Method for Measuring Water Content of Hailstones

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4216089
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    • Journal of Applied Meteorology

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    contributor authorGitlin, Sonia N.
    contributor authorFogler, H. Scott
    contributor authorGoyer, Guy G.
    date accessioned2017-06-09T16:46:49Z
    date available2017-06-09T16:46:49Z
    date copyright1966/10/01
    date issued1966
    identifier issn0021-8952
    identifier otherams-7392.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216089
    description abstractA calorimetric method for measuring the liquid water content of hailstones has been developed. When parameters such as the radiative losses of the system and the changes in heat capacity of the apparatus are eliminated by performing all measurements under identical conditions, the temperature drop is linearly related to the mass of ice melted. For equal masses the temperature drop is smaller if water is present, and there is a linear relationship between the changes in temperature drop and the amount of water present. The water content of hailstones can then be determined from a calibration plot of the changes in temperature drop as a function of the water content of ice.
    publisherAmerican Meteorological Society
    titleA Calorimetric Method for Measuring Water Content of Hailstones
    typeJournal Paper
    journal volume5
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1966)005<0715:ACMFMW>2.0.CO;2
    journal fristpage715
    journal lastpage721
    treeJournal of Applied Meteorology:;1966:;volume( 005 ):;issue: 005
    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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