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    The Small-Particle Response of an Optical Array Precipitation Probe

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 006::page 816
    Author:
    Curry, Michael J.
    ,
    Schemenauer, Robert S.
    DOI: 10.1175/1520-0450(1979)018<0816:TSPROA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The response characteristics of an optical array precipitation spectrometer probe (PMS-OAP-200Y) have been studied in the laboratory using precision glass beads ejected from a specially constructed air gun. The low-end behavior of the probe is described in terms of a high-pass filter characteristic, which can be used to explain the response of the instrument to a particle population having a wide distribution of sizes. It is shown that the particle concentrations measured in channel 1 of the OAP-200Y require correction by a factor which is a function of particle size distribution. For typical experimental situations in rain, the correction factor is approximately 1.8. The remaining size channels do not require correction, provided that the probe sample area and channel width have been properly determined.
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      The Small-Particle Response of an Optical Array Precipitation Probe

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4233243
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    contributor authorCurry, Michael J.
    contributor authorSchemenauer, Robert S.
    date accessioned2017-06-09T17:40:05Z
    date available2017-06-09T17:40:05Z
    date copyright1979/06/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-9723.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233243
    description abstractThe response characteristics of an optical array precipitation spectrometer probe (PMS-OAP-200Y) have been studied in the laboratory using precision glass beads ejected from a specially constructed air gun. The low-end behavior of the probe is described in terms of a high-pass filter characteristic, which can be used to explain the response of the instrument to a particle population having a wide distribution of sizes. It is shown that the particle concentrations measured in channel 1 of the OAP-200Y require correction by a factor which is a function of particle size distribution. For typical experimental situations in rain, the correction factor is approximately 1.8. The remaining size channels do not require correction, provided that the probe sample area and channel width have been properly determined.
    publisherAmerican Meteorological Society
    titleThe Small-Particle Response of an Optical Array Precipitation Probe
    typeJournal Paper
    journal volume18
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1979)018<0816:TSPROA>2.0.CO;2
    journal fristpage816
    journal lastpage821
    treeJournal of Applied Meteorology:;1979:;volume( 018 ):;issue: 006
    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
    yabeshDSpacePersian