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    Satellite Remote Sensing of Multiple Cloud Layers

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 023::page 4210
    Author:
    Baum, B.A.
    ,
    Uttal, T.
    ,
    Poellot, M.
    ,
    Ackerman, T.P.
    ,
    Alvarez, J.M.
    ,
    Intrieri, J.
    ,
    Starr, D.O'C.
    ,
    Titlow, J.
    ,
    Tovinkere, V.
    ,
    Clothiaux, E.
    DOI: 10.1175/1520-0469(1995)052<4210:SRSOMC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The goals of the current study are threefold: 1) to present a multispectral, multiresolution (MSMR) methodology for analysis of scenes containing multiple cloud layers; 2) to apply the MSMR method to two multilevel cloud scenes recorded by the NOAA Advanced Very High Resolution Radiometer (AVHRR) and the High Resolution Infrared Radiometer Sounder (HIRS/2) instruments during the First International Satellite Cloud Climatology Program (ISCCP) Regional Experiment (FIRE) on 28 November 1991; and 3) to validate the cloud-top height results from the case study analyses through comparison with lidar, radar, aircraft and rawin-sonde data. The measurements available from FIRE Cirrus II enable detailed examination of two complex cloud scenes in which cirrus and stratus appear simultaneously. A ?fuzzy logic? classification system is developed to determine whether a 32?32 array of AVHRR data contains clear sky, low-level cloud, midlevel cloud, high-level cloud, or multiple cloud layers. With the addition of the fray logic cloud classification system, it is possible for the first time to find evidence of more than one cloud layer within each HMS field of view. Low cloud heights are determined through application of the spatial coherence method to the AVHRR data, while mid- to high-level cloud heights are calculated from the HIRS/2 15-µm CO2 band radiometric data that are collocated with the AVHRR data. Cirrus cloud heights retrieved from HIRS 15-µm CO2 band data are improved for optically thin cirrus through the use of the upper-tropospheric humidity profile. The MSMR-derived cloud heights are consistent with coincident lidar, radar, and aircraft data. Cirrus and stratus cloud-top heights and cirrus effective emittances are retrieved for data within an ISCCP 2.5° grid cell that encompasses the FIRE experimental region.
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      Satellite Remote Sensing of Multiple Cloud Layers

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4158003
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    • Journal of the Atmospheric Sciences

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    contributor authorBaum, B.A.
    contributor authorUttal, T.
    contributor authorPoellot, M.
    contributor authorAckerman, T.P.
    contributor authorAlvarez, J.M.
    contributor authorIntrieri, J.
    contributor authorStarr, D.O'C.
    contributor authorTitlow, J.
    contributor authorTovinkere, V.
    contributor authorClothiaux, E.
    date accessioned2017-06-09T14:33:34Z
    date available2017-06-09T14:33:34Z
    date copyright1995/12/01
    date issued1995
    identifier issn0022-4928
    identifier otherams-21641.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158003
    description abstractThe goals of the current study are threefold: 1) to present a multispectral, multiresolution (MSMR) methodology for analysis of scenes containing multiple cloud layers; 2) to apply the MSMR method to two multilevel cloud scenes recorded by the NOAA Advanced Very High Resolution Radiometer (AVHRR) and the High Resolution Infrared Radiometer Sounder (HIRS/2) instruments during the First International Satellite Cloud Climatology Program (ISCCP) Regional Experiment (FIRE) on 28 November 1991; and 3) to validate the cloud-top height results from the case study analyses through comparison with lidar, radar, aircraft and rawin-sonde data. The measurements available from FIRE Cirrus II enable detailed examination of two complex cloud scenes in which cirrus and stratus appear simultaneously. A ?fuzzy logic? classification system is developed to determine whether a 32?32 array of AVHRR data contains clear sky, low-level cloud, midlevel cloud, high-level cloud, or multiple cloud layers. With the addition of the fray logic cloud classification system, it is possible for the first time to find evidence of more than one cloud layer within each HMS field of view. Low cloud heights are determined through application of the spatial coherence method to the AVHRR data, while mid- to high-level cloud heights are calculated from the HIRS/2 15-µm CO2 band radiometric data that are collocated with the AVHRR data. Cirrus cloud heights retrieved from HIRS 15-µm CO2 band data are improved for optically thin cirrus through the use of the upper-tropospheric humidity profile. The MSMR-derived cloud heights are consistent with coincident lidar, radar, and aircraft data. Cirrus and stratus cloud-top heights and cirrus effective emittances are retrieved for data within an ISCCP 2.5° grid cell that encompasses the FIRE experimental region.
    publisherAmerican Meteorological Society
    titleSatellite Remote Sensing of Multiple Cloud Layers
    typeJournal Paper
    journal volume52
    journal issue23
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1995)052<4210:SRSOMC>2.0.CO;2
    journal fristpage4210
    journal lastpage4230
    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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