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    Determination of Unfiltered Radiances from the Clouds and the Earth’s Radiant Energy System Instrument

    Source: Journal of Applied Meteorology:;2001:;volume( 040 ):;issue: 004::page 822
    Author:
    Loeb, Norman G.
    ,
    Priestley, Kory J.
    ,
    Kratz, David P.
    ,
    Geier, Erika B.
    ,
    Green, Richard N.
    ,
    Wielicki, Bruce A.
    ,
    Hinton, Patricia O’Rawe
    ,
    Nolan, Sandra K.
    DOI: 10.1175/1520-0450(2001)040<0822:DOURFT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new method for determining unfiltered shortwave (SW), longwave (LW), and window radiances from filtered radiances measured by the Clouds and the Earth?s Radiant Energy System (CERES) satellite instrument is presented. The method uses theoretically derived regression coefficients between filtered and unfiltered radiances that are a function of viewing geometry, geotype, and whether cloud is present. Relative errors in instantaneous unfiltered radiances from this method are generally well below 1% for SW radiances (std dev ≈0.4% or ≈1 W m?2 equivalent flux), less than 0.2% for LW radiances (std dev ≈0.1% or ≈0.3 W m?2 equivalent flux), and less than 0.2% (std dev ≈0.1%) for window channel radiances. When three months (June, July, and August of 1998) of CERES Earth Radiation Budget Experiment (ERBE)-like unfiltered radiances from the Tropical Rainfall Measuring Mission satellite between 20°S and 20°N are compared with archived Earth Radiation Budget Satellite (ERBS) scanner measurements for the same months over a 5-yr period (1985?89), significant scene-type dependent differences are observed in the SW channel. Full-resolution CERES SW unfiltered radiances are ≈7.5% (≈3 W m?2 equivalent diurnal average flux) lower than ERBS over clear ocean, as compared with ≈1.7% (≈4 W m?2 equivalent diurnal average flux) for deep convective clouds and ≈6% (≈4?6 W m?2 equivalent diurnal average flux) for clear land and desert. This dependence on scene type is shown to be partly caused by differences in spatial resolution between CERES and ERBS and by errors in the unfiltering method used in ERBS. When the CERES measurements are spatially averaged to match the ERBS spatial resolution and the unfiltering scheme proposed in this study is applied to both CERES and ERBS, the ERBS all-sky SW radiances increase by ≈1.7%, and the CERES radiances are now consistently ≈3.5%?5% lower than the modified ERBS values for all scene types. Further study is needed to determine the cause for this remaining difference, and even calibration errors cannot be ruled out. CERES LW radiances are closer to ERBS values for individual scene types?CERES radiances are within ≈0.1% (≈0.3 W m?2) of ERBS over clear ocean and ≈0.5% (≈1.5 W m?2) over clear land and desert.
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      Determination of Unfiltered Radiances from the Clouds and the Earth’s Radiant Energy System Instrument

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148387
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    • Journal of Applied Meteorology

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    contributor authorLoeb, Norman G.
    contributor authorPriestley, Kory J.
    contributor authorKratz, David P.
    contributor authorGeier, Erika B.
    contributor authorGreen, Richard N.
    contributor authorWielicki, Bruce A.
    contributor authorHinton, Patricia O’Rawe
    contributor authorNolan, Sandra K.
    date accessioned2017-06-09T14:07:49Z
    date available2017-06-09T14:07:49Z
    date copyright2001/04/01
    date issued2001
    identifier issn0894-8763
    identifier otherams-12988.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148387
    description abstractA new method for determining unfiltered shortwave (SW), longwave (LW), and window radiances from filtered radiances measured by the Clouds and the Earth?s Radiant Energy System (CERES) satellite instrument is presented. The method uses theoretically derived regression coefficients between filtered and unfiltered radiances that are a function of viewing geometry, geotype, and whether cloud is present. Relative errors in instantaneous unfiltered radiances from this method are generally well below 1% for SW radiances (std dev ≈0.4% or ≈1 W m?2 equivalent flux), less than 0.2% for LW radiances (std dev ≈0.1% or ≈0.3 W m?2 equivalent flux), and less than 0.2% (std dev ≈0.1%) for window channel radiances. When three months (June, July, and August of 1998) of CERES Earth Radiation Budget Experiment (ERBE)-like unfiltered radiances from the Tropical Rainfall Measuring Mission satellite between 20°S and 20°N are compared with archived Earth Radiation Budget Satellite (ERBS) scanner measurements for the same months over a 5-yr period (1985?89), significant scene-type dependent differences are observed in the SW channel. Full-resolution CERES SW unfiltered radiances are ≈7.5% (≈3 W m?2 equivalent diurnal average flux) lower than ERBS over clear ocean, as compared with ≈1.7% (≈4 W m?2 equivalent diurnal average flux) for deep convective clouds and ≈6% (≈4?6 W m?2 equivalent diurnal average flux) for clear land and desert. This dependence on scene type is shown to be partly caused by differences in spatial resolution between CERES and ERBS and by errors in the unfiltering method used in ERBS. When the CERES measurements are spatially averaged to match the ERBS spatial resolution and the unfiltering scheme proposed in this study is applied to both CERES and ERBS, the ERBS all-sky SW radiances increase by ≈1.7%, and the CERES radiances are now consistently ≈3.5%?5% lower than the modified ERBS values for all scene types. Further study is needed to determine the cause for this remaining difference, and even calibration errors cannot be ruled out. CERES LW radiances are closer to ERBS values for individual scene types?CERES radiances are within ≈0.1% (≈0.3 W m?2) of ERBS over clear ocean and ≈0.5% (≈1.5 W m?2) over clear land and desert.
    publisherAmerican Meteorological Society
    titleDetermination of Unfiltered Radiances from the Clouds and the Earth’s Radiant Energy System Instrument
    typeJournal Paper
    journal volume40
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2001)040<0822:DOURFT>2.0.CO;2
    journal fristpage822
    journal lastpage835
    treeJournal of Applied Meteorology:;2001:;volume( 040 ):;issue: 004
    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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