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    Angular Truncation Error of the Integrating Nephelometer in the Fog Droplet Size Range

    Source: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 002::page 208
    Author:
    Fitzgerald, James W.
    DOI: 10.1175/1520-0450(1977)016<0210:ATEOTI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Integrating nephelometers have an inherent error, known as the angular truncation error, which arises from the fact that they integrate scattered light intensity over a truncated angular range from ?1 > 0° to ?2 < 180°. Typically, ?1 is between 5° and 10°. Since the proportion of light scattered in the extreme forward direction increases as scatterer size increases, this error can become sizeable for measurements made in fogs. Correction factors ?(α) for angular truncation are computed for spherical water droplets having values of the size parameter α (= πd/?) in the range 3?200, for values of ?1 of 6°?9° and for ?2 = 170°. If monochromatic light of wavelength 0.55 ?m is assumed, this range of α corresponds to droplet diameters between 0.53 and 35 ?m. The magnitude of ?(α) increases nonmonotonically from a value between 1.03 and 1.07 (depending on ?1) for α = 3 to a value between 2.0 and 2.14 for α = 100. In the range 100 < α ≤ 200, ?(α) varies by less than 7%. Angular truncation correction factors applicable to the MRI model 1580 Fog Visinmeter are also computed.
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      Angular Truncation Error of the Integrating Nephelometer in the Fog Droplet Size Range

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4232704
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    contributor authorFitzgerald, James W.
    date accessioned2017-06-09T17:38:58Z
    date available2017-06-09T17:38:58Z
    date copyright1977/02/01
    date issued1977
    identifier issn0021-8952
    identifier otherams-9238.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232704
    description abstractIntegrating nephelometers have an inherent error, known as the angular truncation error, which arises from the fact that they integrate scattered light intensity over a truncated angular range from ?1 > 0° to ?2 < 180°. Typically, ?1 is between 5° and 10°. Since the proportion of light scattered in the extreme forward direction increases as scatterer size increases, this error can become sizeable for measurements made in fogs. Correction factors ?(α) for angular truncation are computed for spherical water droplets having values of the size parameter α (= πd/?) in the range 3?200, for values of ?1 of 6°?9° and for ?2 = 170°. If monochromatic light of wavelength 0.55 ?m is assumed, this range of α corresponds to droplet diameters between 0.53 and 35 ?m. The magnitude of ?(α) increases nonmonotonically from a value between 1.03 and 1.07 (depending on ?1) for α = 3 to a value between 2.0 and 2.14 for α = 100. In the range 100 < α ≤ 200, ?(α) varies by less than 7%. Angular truncation correction factors applicable to the MRI model 1580 Fog Visinmeter are also computed.
    publisherAmerican Meteorological Society
    titleAngular Truncation Error of the Integrating Nephelometer in the Fog Droplet Size Range
    typeJournal Paper
    journal volume16
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1977)016<0210:ATEOTI>2.0.CO;2
    journal fristpage208
    journal lastpage213
    treeJournal of Applied Meteorology:;1977:;volume( 016 ):;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
    yabeshDSpacePersian