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    Measurements of Atmospheric Extinction in the Spectral Region 360–800 nm by Spectroradiometry

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 004::page 603
    Author:
    Steinvall, Ove
    ,
    Hugo Ågren, Carl
    DOI: 10.1175/1520-0450(1975)014<0603:MOAEIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Measurements of atmospheric extinction in the spectral region 330?803 nm have been made by measuring the apparent radiance of a hole in a black box and relating this to the radiance of the horizon sky. The spectroradiometer used for this was bat at our institute. Good correlation was achieved between the extinction coefficient at 500 nm measured in this way and the scattering coefficient wavelength measured with a nephelometer. The wavelength dependence of the extinction was in most cases in agreement with Ångström's power law with the extinction coefficient bext ? ??α. Typical values of α were in the interval 0.75 ≤ α ≤ 1.5. The influence of the relative humidity on α and on the extinction has been studied.
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      Measurements of Atmospheric Extinction in the Spectral Region 360–800 nm by Spectroradiometry

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4232307
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    contributor authorSteinvall, Ove
    contributor authorHugo Ågren, Carl
    date accessioned2017-06-09T17:38:09Z
    date available2017-06-09T17:38:09Z
    date copyright1975/06/01
    date issued1975
    identifier issn0021-8952
    identifier otherams-8881.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232307
    description abstractMeasurements of atmospheric extinction in the spectral region 330?803 nm have been made by measuring the apparent radiance of a hole in a black box and relating this to the radiance of the horizon sky. The spectroradiometer used for this was bat at our institute. Good correlation was achieved between the extinction coefficient at 500 nm measured in this way and the scattering coefficient wavelength measured with a nephelometer. The wavelength dependence of the extinction was in most cases in agreement with Ångström's power law with the extinction coefficient bext ? ??α. Typical values of α were in the interval 0.75 ≤ α ≤ 1.5. The influence of the relative humidity on α and on the extinction has been studied.
    publisherAmerican Meteorological Society
    titleMeasurements of Atmospheric Extinction in the Spectral Region 360–800 nm by Spectroradiometry
    typeJournal Paper
    journal volume14
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1975)014<0603:MOAEIT>2.0.CO;2
    journal fristpage603
    journal lastpage608
    treeJournal of Applied Meteorology:;1975:;volume( 014 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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