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    The Absorption of Solar Radiation by Cloud Droplets: An Application of Anomalous Diffraction Theory

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 012::page 1574
    Author:
    Ackerman, Steven A.
    ,
    Stephens, Graeme L.
    DOI: 10.1175/1520-0469(1987)044<1574:TAOSRB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper we demonstrate that the anomalous diffraction theory of van de Hulst with some modifications, provides a reasonable approximation of the volume extinction and absorption coefficients. We also show how the shortwave radiative properties of a water cloud can be derived in terms of 1) cloud liquid water path, 2) the effective radius of the droplet distribution, and 3) the balk absorption coefficient of water. With the aid of the approximate diffraction theory we describe how cloud albedo and shortwave absorption depend on the droplet size. We demonstrate this dependence to be somewhat complex and show that the variation of absorption with variation of droplet size depends also on the cloud liquid water path. For ?deep? or semi-infinite clouds, absorption increases monotonically with increasing effective radius, but the reverse dependence is established for thin clouds. The implications of these results to the so-called absorption paradox and to the possibility of determining droplet size information from remotely measured reflectance spectra are also discussed.
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      The Absorption of Solar Radiation by Cloud Droplets: An Application of Anomalous Diffraction Theory

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155681
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    contributor authorAckerman, Steven A.
    contributor authorStephens, Graeme L.
    date accessioned2017-06-09T14:27:23Z
    date available2017-06-09T14:27:23Z
    date copyright1987/06/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19552.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155681
    description abstractIn this paper we demonstrate that the anomalous diffraction theory of van de Hulst with some modifications, provides a reasonable approximation of the volume extinction and absorption coefficients. We also show how the shortwave radiative properties of a water cloud can be derived in terms of 1) cloud liquid water path, 2) the effective radius of the droplet distribution, and 3) the balk absorption coefficient of water. With the aid of the approximate diffraction theory we describe how cloud albedo and shortwave absorption depend on the droplet size. We demonstrate this dependence to be somewhat complex and show that the variation of absorption with variation of droplet size depends also on the cloud liquid water path. For ?deep? or semi-infinite clouds, absorption increases monotonically with increasing effective radius, but the reverse dependence is established for thin clouds. The implications of these results to the so-called absorption paradox and to the possibility of determining droplet size information from remotely measured reflectance spectra are also discussed.
    publisherAmerican Meteorological Society
    titleThe Absorption of Solar Radiation by Cloud Droplets: An Application of Anomalous Diffraction Theory
    typeJournal Paper
    journal volume44
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<1574:TAOSRB>2.0.CO;2
    journal fristpage1574
    journal lastpage1588
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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