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    Remote Sounding of Cirrus Cloud Optical Depths and Ice Crystal Sizes from AVHRR Data: Verification Using FIRE II IFO Measurements

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 023::page 4143
    Author:
    Ou, S.C.
    ,
    Liou, K.N.
    ,
    Takano, Y.
    ,
    Rao, N.X.
    ,
    Fu, Q.
    ,
    Heymsfield, A.J.
    ,
    Miloshevich, L.M.
    ,
    Baum, B.
    ,
    Kinne, S.A.
    DOI: 10.1175/1520-0469(1995)052<4143:RSOCCO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Using the data obtained from the Advanced Very High Resolution Radiometer (AVHRR) 3.7-µm and 10.9-µm channels, a retrieval scheme has been developed to simultaneously infer cirrus cloud optical depth and mean effective ice crystal size based on the theory of radiative transfer and parameterizations. A numerical scheme is further developed to remove the solar component in the 3.7-µm radiance for applications to daytime satellite data. This scheme is based on the correlation between the 3.7-µm (solar) and 0.63-µm reflectances. Validation of the algorithm has been performed by using various datasets that were collected during the FIRE-II IFO (Nov-Dec 1991) at Coffeyville, Kansas. We have focused on the 26 November and 5 December cases. The retrieval analysis over a 0.5°?1.0° area is performed around Coffeyville for each case based on AVHRR-HRPT data. For validation the authors analyze the photomicrograph data collected by the balloonborne replicator, determine the microphysical and optical properties of the sampled cirrus clouds, and derive their position at the satellite overpass based on sounding data. It is demonstrated that the retrieved cirrus cloud temperature, mean effective ice crystal size, and optical depth closely match the observed values. Further, the retrieved cirrus cloud properties are applied to the computation of surface radiative fluxes using a radiative transfer program that involves a consistent representation of cirrus cloud fields. The computed values are compared with the data measured from ground-based radiometers, and it is shown that the computed downward surface IR and solar fluxes are within 5 and 10 W m?2 of the measured values, respectively, near the time of satellite overpass.
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      Remote Sounding of Cirrus Cloud Optical Depths and Ice Crystal Sizes from AVHRR Data: Verification Using FIRE II IFO Measurements

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157998
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    • Journal of the Atmospheric Sciences

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    contributor authorOu, S.C.
    contributor authorLiou, K.N.
    contributor authorTakano, Y.
    contributor authorRao, N.X.
    contributor authorFu, Q.
    contributor authorHeymsfield, A.J.
    contributor authorMiloshevich, L.M.
    contributor authorBaum, B.
    contributor authorKinne, S.A.
    date accessioned2017-06-09T14:33:33Z
    date available2017-06-09T14:33:33Z
    date copyright1995/12/01
    date issued1995
    identifier issn0022-4928
    identifier otherams-21637.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157998
    description abstractUsing the data obtained from the Advanced Very High Resolution Radiometer (AVHRR) 3.7-µm and 10.9-µm channels, a retrieval scheme has been developed to simultaneously infer cirrus cloud optical depth and mean effective ice crystal size based on the theory of radiative transfer and parameterizations. A numerical scheme is further developed to remove the solar component in the 3.7-µm radiance for applications to daytime satellite data. This scheme is based on the correlation between the 3.7-µm (solar) and 0.63-µm reflectances. Validation of the algorithm has been performed by using various datasets that were collected during the FIRE-II IFO (Nov-Dec 1991) at Coffeyville, Kansas. We have focused on the 26 November and 5 December cases. The retrieval analysis over a 0.5°?1.0° area is performed around Coffeyville for each case based on AVHRR-HRPT data. For validation the authors analyze the photomicrograph data collected by the balloonborne replicator, determine the microphysical and optical properties of the sampled cirrus clouds, and derive their position at the satellite overpass based on sounding data. It is demonstrated that the retrieved cirrus cloud temperature, mean effective ice crystal size, and optical depth closely match the observed values. Further, the retrieved cirrus cloud properties are applied to the computation of surface radiative fluxes using a radiative transfer program that involves a consistent representation of cirrus cloud fields. The computed values are compared with the data measured from ground-based radiometers, and it is shown that the computed downward surface IR and solar fluxes are within 5 and 10 W m?2 of the measured values, respectively, near the time of satellite overpass.
    publisherAmerican Meteorological Society
    titleRemote Sounding of Cirrus Cloud Optical Depths and Ice Crystal Sizes from AVHRR Data: Verification Using FIRE II IFO Measurements
    typeJournal Paper
    journal volume52
    journal issue23
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1995)052<4143:RSOCCO>2.0.CO;2
    journal fristpage4143
    journal lastpage4158
    treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 023
    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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