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    The Role of Clear-Sky Identification in the Study of Cloud Radiative Effects: Combined Analysis from ISCCP and the Scanner of Radiation Budget

    Source: Journal of Applied Meteorology:;2002:;volume( 041 ):;issue: 004::page 396
    Author:
    Stubenrauch, C. J.
    ,
    Briand, V.
    ,
    Rossow, W. B.
    DOI: 10.1175/1520-0450(2002)041<0396:TROCSI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Two additional narrowband channels of the Scanner of Radiation Budget (ScaRaB) instrument should improve the Earth Radiation Budget Experiment (ERBE) cloud scene identification. Applying the original International Satellite Cloud Climatology Project (ISCCP) algorithms to the ScaRaB narrowband data gives a clear-sky frequency that is about 5% lower than that given by quasi-simultaneous ISCCP data, an indication that the ISCCP cloud detection is very stable. However, one would expect about 10%?20% smaller clear-sky occurrence for the larger ScaRaB pixels. Adapting the ISCCP algorithms to the ScaRaB spatial resolution and to the different time sampling of the ScaRaB data leads to a reduction of residual cloud contamination. A sensitivity study with time?space-collocated ScaRaB and ISCCP data shows that the clear-sky identification method has a greater effect on the clear-sky frequency and therefore on the statistics than on the zonal mean values of the clear-sky fluxes. The zonal outgoing longwave (LW) fluxes corresponding to ERBE clear sky are in general about 2?10 W m?2 higher than those from the ScaRaB-adapted ISCCP clear-sky identifications. The latter are close to fluxes corresponding to clear-sky regions from ISCCP data, whereas ScaRaB clear-sky LW fluxes obtained with the original ISCCP identification lie about 1?2 W m?2 below. Especially in the Tropics, where water vapor abundance is high, the ERBE clear-sky LW fluxes seem to be systematically overestimated by about 4 W m?2, and shortwave (SW) fluxes are lower by about 5?10 W m?2. However, another source of uncertainty in the monthly mean zonal cloud radiative effects comes from the low frequency of clear-sky occurrence, when averaging over regions that correspond to the spatial resolution of general circulation models. An additional systematic sampling bias in the clear-sky fluxes appears because the clear-sky regions selected by the different algorithms occur in different geographic regions with different cloud properties.
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      The Role of Clear-Sky Identification in the Study of Cloud Radiative Effects: Combined Analysis from ISCCP and the Scanner of Radiation Budget

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148553
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    contributor authorStubenrauch, C. J.
    contributor authorBriand, V.
    contributor authorRossow, W. B.
    date accessioned2017-06-09T14:08:22Z
    date available2017-06-09T14:08:22Z
    date copyright2002/04/01
    date issued2002
    identifier issn0894-8763
    identifier otherams-13136.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148553
    description abstractTwo additional narrowband channels of the Scanner of Radiation Budget (ScaRaB) instrument should improve the Earth Radiation Budget Experiment (ERBE) cloud scene identification. Applying the original International Satellite Cloud Climatology Project (ISCCP) algorithms to the ScaRaB narrowband data gives a clear-sky frequency that is about 5% lower than that given by quasi-simultaneous ISCCP data, an indication that the ISCCP cloud detection is very stable. However, one would expect about 10%?20% smaller clear-sky occurrence for the larger ScaRaB pixels. Adapting the ISCCP algorithms to the ScaRaB spatial resolution and to the different time sampling of the ScaRaB data leads to a reduction of residual cloud contamination. A sensitivity study with time?space-collocated ScaRaB and ISCCP data shows that the clear-sky identification method has a greater effect on the clear-sky frequency and therefore on the statistics than on the zonal mean values of the clear-sky fluxes. The zonal outgoing longwave (LW) fluxes corresponding to ERBE clear sky are in general about 2?10 W m?2 higher than those from the ScaRaB-adapted ISCCP clear-sky identifications. The latter are close to fluxes corresponding to clear-sky regions from ISCCP data, whereas ScaRaB clear-sky LW fluxes obtained with the original ISCCP identification lie about 1?2 W m?2 below. Especially in the Tropics, where water vapor abundance is high, the ERBE clear-sky LW fluxes seem to be systematically overestimated by about 4 W m?2, and shortwave (SW) fluxes are lower by about 5?10 W m?2. However, another source of uncertainty in the monthly mean zonal cloud radiative effects comes from the low frequency of clear-sky occurrence, when averaging over regions that correspond to the spatial resolution of general circulation models. An additional systematic sampling bias in the clear-sky fluxes appears because the clear-sky regions selected by the different algorithms occur in different geographic regions with different cloud properties.
    publisherAmerican Meteorological Society
    titleThe Role of Clear-Sky Identification in the Study of Cloud Radiative Effects: Combined Analysis from ISCCP and the Scanner of Radiation Budget
    typeJournal Paper
    journal volume41
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2002)041<0396:TROCSI>2.0.CO;2
    journal fristpage396
    journal lastpage412
    treeJournal of Applied Meteorology:;2002:;volume( 041 ):;issue: 004
    contenttypeFulltext
    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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian