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    Airborne Spectral Measurements of Ocean Directional Reflectance

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 004::page 1072
    Author:
    Gatebe, Charles K.
    ,
    King, Michael D.
    ,
    Lyapustin, Alexei I.
    ,
    Arnold, G. Thomas
    ,
    Redemann, Jens
    DOI: 10.1175/JAS3386.1
    Publisher: American Meteorological Society
    Abstract: The Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BRDF) of the ocean in July and August 2001 under different illumination conditions with solar zenith angles ranging from 15° to 46°. The BRDF measurements were accompanied by concurrent measurements of atmospheric aerosol optical thickness and column water vapor above the airplane. The method of spherical harmonics with Cox?Munk wave-slope distribution is used in a new algorithm developed for this study to solve the atmosphere?ocean radiative transfer problem and to remove the effects of the atmosphere from airborne measurements. The algorithm retrieves simultaneously the wind speed and full ocean BRDF (sun?s glitter and water-leaving radiance) from CAR measurements and evaluates total albedo and equivalent albedo for the water-leaving radiance outside the glitter. Results show good overall agreement with other measurements and theoretical simulations, with the anisotropy of the water-leaving radiance clearly seen. However, the water-leaving radiance does not show a strong dependence on solar zenith angle as suggested by some theoretical studies. The spectral albedo was found to vary from 4.1%?5.1% at ? = 0.472 ?m to 2.4%?3.5% for ? ≥ 0.682 ?m. The equivalent water-leaving albedo ranges from 1.0%?2.4% at ? = 0.472 ?m to 0.1%?0.6% for ? = 0.682 ?m and 0.1%?0.3% for ? = 0.870 ?m. Results of the validation of the Cox?Munk model under the conditions measured show that although the model reproduces the shape of sun?s glitter on average with an accuracy of better than 30%, it underestimates the center of the sun?s glitter reflectance by about 30% for low wind speeds (<2?3 m s?1). In cases of high wind speed, the model with Gram?Charlier expansion seems to provide the best fit.
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      Airborne Spectral Measurements of Ocean Directional Reflectance

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4217925
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    • Journal of the Atmospheric Sciences

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    contributor authorGatebe, Charles K.
    contributor authorKing, Michael D.
    contributor authorLyapustin, Alexei I.
    contributor authorArnold, G. Thomas
    contributor authorRedemann, Jens
    date accessioned2017-06-09T16:52:02Z
    date available2017-06-09T16:52:02Z
    date copyright2005/04/01
    date issued2005
    identifier issn0022-4928
    identifier otherams-75574.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217925
    description abstractThe Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BRDF) of the ocean in July and August 2001 under different illumination conditions with solar zenith angles ranging from 15° to 46°. The BRDF measurements were accompanied by concurrent measurements of atmospheric aerosol optical thickness and column water vapor above the airplane. The method of spherical harmonics with Cox?Munk wave-slope distribution is used in a new algorithm developed for this study to solve the atmosphere?ocean radiative transfer problem and to remove the effects of the atmosphere from airborne measurements. The algorithm retrieves simultaneously the wind speed and full ocean BRDF (sun?s glitter and water-leaving radiance) from CAR measurements and evaluates total albedo and equivalent albedo for the water-leaving radiance outside the glitter. Results show good overall agreement with other measurements and theoretical simulations, with the anisotropy of the water-leaving radiance clearly seen. However, the water-leaving radiance does not show a strong dependence on solar zenith angle as suggested by some theoretical studies. The spectral albedo was found to vary from 4.1%?5.1% at ? = 0.472 ?m to 2.4%?3.5% for ? ≥ 0.682 ?m. The equivalent water-leaving albedo ranges from 1.0%?2.4% at ? = 0.472 ?m to 0.1%?0.6% for ? = 0.682 ?m and 0.1%?0.3% for ? = 0.870 ?m. Results of the validation of the Cox?Munk model under the conditions measured show that although the model reproduces the shape of sun?s glitter on average with an accuracy of better than 30%, it underestimates the center of the sun?s glitter reflectance by about 30% for low wind speeds (<2?3 m s?1). In cases of high wind speed, the model with Gram?Charlier expansion seems to provide the best fit.
    publisherAmerican Meteorological Society
    titleAirborne Spectral Measurements of Ocean Directional Reflectance
    typeJournal Paper
    journal volume62
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS3386.1
    journal fristpage1072
    journal lastpage1092
    treeJournal of the Atmospheric Sciences:;2005:;Volume( 062 ):;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
    yabeshDSpacePersian