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    Time-Resolved Measurement of Droplet Size and Concentration in Cloud Chambers

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 004::page 684
    Author:
    Cole, J. E.
    ,
    Dobbins, R. A.
    ,
    Semerjian, H.
    DOI: 10.1175/1520-0450(1970)009<0684:TRMODS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An optical method for measuring droplet size and concentration in a cloud chamber on a time-resolved basis is discussed. During the growth of the droplets, speed transmission at two wavelengths of light is continuously measured by high-speed electronic equipment. Interpretation of the resulting transmission vs time curves is made on the bash of Mie muttering theory. The appearance of oscillatory regions in the transmission curves is related to the primary oscillations of the scattering coefficient and indicates the presence of a monodisperse cloud. Two methods of data interpretation are discussed from which absolute values of droplet silt and concentration are obtained. Final droplet diameters from 1.75?10.4 ?m with corresponding concentrations from 1.80 ? 106?1.15 ? 104 cm?3 have been measured in our cloud chamber. The technique is applicable to condensation studies conducted in Wilson cloud chambers. We suggest that apparatus of the type described is also suitable for the absolute calibration of condensation nuclei counters of various types.
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      Time-Resolved Measurement of Droplet Size and Concentration in Cloud Chambers

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4223234
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    • Journal of Applied Meteorology

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    contributor authorCole, J. E.
    contributor authorDobbins, R. A.
    contributor authorSemerjian, H.
    date accessioned2017-06-09T17:09:42Z
    date available2017-06-09T17:09:42Z
    date copyright1970/08/01
    date issued1970
    identifier issn0021-8952
    identifier otherams-8035.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223234
    description abstractAn optical method for measuring droplet size and concentration in a cloud chamber on a time-resolved basis is discussed. During the growth of the droplets, speed transmission at two wavelengths of light is continuously measured by high-speed electronic equipment. Interpretation of the resulting transmission vs time curves is made on the bash of Mie muttering theory. The appearance of oscillatory regions in the transmission curves is related to the primary oscillations of the scattering coefficient and indicates the presence of a monodisperse cloud. Two methods of data interpretation are discussed from which absolute values of droplet silt and concentration are obtained. Final droplet diameters from 1.75?10.4 ?m with corresponding concentrations from 1.80 ? 106?1.15 ? 104 cm?3 have been measured in our cloud chamber. The technique is applicable to condensation studies conducted in Wilson cloud chambers. We suggest that apparatus of the type described is also suitable for the absolute calibration of condensation nuclei counters of various types.
    publisherAmerican Meteorological Society
    titleTime-Resolved Measurement of Droplet Size and Concentration in Cloud Chambers
    typeJournal Paper
    journal volume9
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1970)009<0684:TRMODS>2.0.CO;2
    journal fristpage684
    journal lastpage689
    treeJournal of Applied Meteorology:;1970:;volume( 009 ):;issue: 004
    contenttypeFulltext
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