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    Aerosol Remote Sensing over Clouds Using A-Train Observations

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008::page 2468
    Author:
    Waquet, F.
    ,
    Riedi, J.
    ,
    Labonnote, L. C.
    ,
    Goloub, P.
    ,
    Cairns, B.
    ,
    Deuzé, J-L.
    ,
    Tanré, D.
    DOI: 10.1175/2009JAS3026.1
    Publisher: American Meteorological Society
    Abstract: The detection of aerosol above clouds is critical for the estimate of both the aerosol and cloud radiative impacts. In this study, the authors present a new method to retrieve the aerosol properties over clouds that uses the multiangle polarization measurements of the Polarization and Directionality of Earth Reflectances (POLDER)?Polarization and Anisotropy of Reflectances for Atmospheric Sciences Coupled with Observations from a Lidar (PARASOL) instrument. The method is illustrated and applied to a case study exploiting the coincident observations from other passive and active sensors of the NASA A-Train satellite constellation. The case study is relative to an elevated biomass burning aerosol layer that originates from southern Africa and is then transported over low-level clouds extending over the Atlantic Ocean. It is shown that the comparison between the cloud-top heights retrieved with the different passive techniques developed for the A-Train sensors can be used to detect the presence of aerosols above clouds. The analysis of the PARASOL observations showed that the aerosols significantly affect the polarized light reflected by the clouds over the 80°?120° scattering angle range and in the rainbow region. A single scattering model permitted the reproduction of the polarization observations and the retrieval of an estimate of the aerosol layer optical thickness of 0.225 at 0.865 ?m. The retrieved aerosol optical thicknesses over clouds agree quantitatively with the closest ones retrieved over clear-sky ocean (±0.04 as a maximum departure), demonstrating the value of the method. This innovative technique based solely on passive measurements is expected to provide a better understanding of aerosol properties in regions where significant cloud cover usually prevents the retrieval of aerosol optical thickness. As such, this new retrieval method can provide significant and valuable information about the radiative impact of clouds and aerosols, especially where they can potentially interact strongly with each other.
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      Aerosol Remote Sensing over Clouds Using A-Train Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4210018
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    contributor authorWaquet, F.
    contributor authorRiedi, J.
    contributor authorLabonnote, L. C.
    contributor authorGoloub, P.
    contributor authorCairns, B.
    contributor authorDeuzé, J-L.
    contributor authorTanré, D.
    date accessioned2017-06-09T16:28:16Z
    date available2017-06-09T16:28:16Z
    date copyright2009/08/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-68458.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210018
    description abstractThe detection of aerosol above clouds is critical for the estimate of both the aerosol and cloud radiative impacts. In this study, the authors present a new method to retrieve the aerosol properties over clouds that uses the multiangle polarization measurements of the Polarization and Directionality of Earth Reflectances (POLDER)?Polarization and Anisotropy of Reflectances for Atmospheric Sciences Coupled with Observations from a Lidar (PARASOL) instrument. The method is illustrated and applied to a case study exploiting the coincident observations from other passive and active sensors of the NASA A-Train satellite constellation. The case study is relative to an elevated biomass burning aerosol layer that originates from southern Africa and is then transported over low-level clouds extending over the Atlantic Ocean. It is shown that the comparison between the cloud-top heights retrieved with the different passive techniques developed for the A-Train sensors can be used to detect the presence of aerosols above clouds. The analysis of the PARASOL observations showed that the aerosols significantly affect the polarized light reflected by the clouds over the 80°?120° scattering angle range and in the rainbow region. A single scattering model permitted the reproduction of the polarization observations and the retrieval of an estimate of the aerosol layer optical thickness of 0.225 at 0.865 ?m. The retrieved aerosol optical thicknesses over clouds agree quantitatively with the closest ones retrieved over clear-sky ocean (±0.04 as a maximum departure), demonstrating the value of the method. This innovative technique based solely on passive measurements is expected to provide a better understanding of aerosol properties in regions where significant cloud cover usually prevents the retrieval of aerosol optical thickness. As such, this new retrieval method can provide significant and valuable information about the radiative impact of clouds and aerosols, especially where they can potentially interact strongly with each other.
    publisherAmerican Meteorological Society
    titleAerosol Remote Sensing over Clouds Using A-Train Observations
    typeJournal Paper
    journal volume66
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2009JAS3026.1
    journal fristpage2468
    journal lastpage2480
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008
    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
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