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    Degradation of In-Cloud Forward Scattering Spectrometer Probe Measurements in the Presence of Ice Particles

    Source: Journal of Atmospheric and Oceanic Technology:;1985:;volume( 002 ):;issue: 002::page 171
    Author:
    Gardiner, B. A.
    ,
    Hallett, J.
    DOI: 10.1175/1520-0426(1985)002<0171:DOICFS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Airborne measurements of cloud liquid water content derived from a formvar replicator, a Johnson-Williams probe and a forward scattering spectrometer probe (FSSP) are compared. These show that in the presence of ice crystals the FSSP droplet spectra may be artificially enhanced. Typically the ice produces a flat distribution superimposed on the actual droplet distribution. The concentrations measured by the FSSP in the presence of ice are found to be 2?3 orders of magnitude greater than the actual ice concentrations as measured by the formvar replicator and a 2D-C probe. Possible explanations for the abnormal behavior of the FSSP in the presence of ice particles are discussed.
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      Degradation of In-Cloud Forward Scattering Spectrometer Probe Measurements in the Presence of Ice Particles

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146623
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorGardiner, B. A.
    contributor authorHallett, J.
    date accessioned2017-06-09T14:02:34Z
    date available2017-06-09T14:02:34Z
    date copyright1985/06/01
    date issued1985
    identifier issn0739-0572
    identifier otherams-114.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146623
    description abstractAirborne measurements of cloud liquid water content derived from a formvar replicator, a Johnson-Williams probe and a forward scattering spectrometer probe (FSSP) are compared. These show that in the presence of ice crystals the FSSP droplet spectra may be artificially enhanced. Typically the ice produces a flat distribution superimposed on the actual droplet distribution. The concentrations measured by the FSSP in the presence of ice are found to be 2?3 orders of magnitude greater than the actual ice concentrations as measured by the formvar replicator and a 2D-C probe. Possible explanations for the abnormal behavior of the FSSP in the presence of ice particles are discussed.
    publisherAmerican Meteorological Society
    titleDegradation of In-Cloud Forward Scattering Spectrometer Probe Measurements in the Presence of Ice Particles
    typeJournal Paper
    journal volume2
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1985)002<0171:DOICFS>2.0.CO;2
    journal fristpage171
    journal lastpage180
    treeJournal of Atmospheric and Oceanic Technology:;1985:;volume( 002 ):;issue: 002
    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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