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    Determination of the Ground Albedo and the Index of Absorption of Atmospheric Particulates by Remote Sensing. Part II:. Application

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 006::page 1072
    Author:
    King, Michael D.
    DOI: 10.1175/1520-0469(1979)036<1072:DOTGAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A hemispherical radiometer has been used to obtain spectrally narrow-band measurements of the downward hemispheric diffuse and total (global) flux densities at varying solar zenith angles on 14 days over Tucson. Data are presented which illustrate the effects of temporally varying atmospheric conditions as well as clear stable conditions on the ratio of the diffuse to direct solar radiation at the earth's surface. The ground albedo and the effective imaginary term of the complex refractive index of atmospheric particulates are derived from the diffuse-direct ratio measurements on seven clear stable days at two wavelengths using the statistical procedure described by King and Herman (1979). Results indicate that the downwelling diffuse radiation field in the mid-visible region in Tucson can be adequately described by Mie scattering theory if the ground albedo is 0.279±0.100 and the index of absorption is 0.0306±0.0082.
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      Determination of the Ground Albedo and the Index of Absorption of Atmospheric Particulates by Remote Sensing. Part II:. Application

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153640
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    contributor authorKing, Michael D.
    date accessioned2017-06-09T14:20:50Z
    date available2017-06-09T14:20:50Z
    date copyright1979/06/01
    date issued1979
    identifier issn0022-4928
    identifier otherams-17715.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153640
    description abstractA hemispherical radiometer has been used to obtain spectrally narrow-band measurements of the downward hemispheric diffuse and total (global) flux densities at varying solar zenith angles on 14 days over Tucson. Data are presented which illustrate the effects of temporally varying atmospheric conditions as well as clear stable conditions on the ratio of the diffuse to direct solar radiation at the earth's surface. The ground albedo and the effective imaginary term of the complex refractive index of atmospheric particulates are derived from the diffuse-direct ratio measurements on seven clear stable days at two wavelengths using the statistical procedure described by King and Herman (1979). Results indicate that the downwelling diffuse radiation field in the mid-visible region in Tucson can be adequately described by Mie scattering theory if the ground albedo is 0.279±0.100 and the index of absorption is 0.0306±0.0082.
    publisherAmerican Meteorological Society
    titleDetermination of the Ground Albedo and the Index of Absorption of Atmospheric Particulates by Remote Sensing. Part II:. Application
    typeJournal Paper
    journal volume36
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1979)036<1072:DOTGAA>2.0.CO;2
    journal fristpage1072
    journal lastpage1083
    treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;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