摘要
High-resolutionspectralradiancemeasurementsweretakenbyaspectralradiometeronboardahelicopterovertheUSOklahomaSouthernGreatPlainneartheAtmosphericRadiationMeasurements(ARM)siteduringAugust1998.Theradiometerhasaspectralrangefrom350nmto2500nmat1nmresolution.Themeasurementscoveredseveralgrassandcroplandscenetypesatmultiplesolarzenithangles.DetailedatmosphericcorrectionsusingtheModerateResolutionTransmittance(MODTRAN)radiationmodelandin-situsoundingandaerosolmeasurementshavebeenappliedtothehelicoptermeasurementsinordertoretrievethesurfaceandtopofatmosphere(TOA)BidirectionalReflectanceDistributionFunction(BRDF)characteristics.Theatmosphericcorrectionsaremostsignificantinthevisiblewavelengthsandinthestrongwatervaporabsorptionwavelengthsinthenearinfraredregion.AdjustingtheBRDFtoTOArequiresalargercorrectioninthevisiblechannelssinceRayleighscatteringcontributessignificantlytotheTOAreflectance.Theoppositecorrectionstothevisibleandnearinfrarredwavelengthscanaltertheradiancedifferenceandratiothatmanyremotesensingtechniquesarebasedon,suchasthenormalizeddifferencevegetationindex(NDVI).ThedatashowthatsurfaceBRDFsandspectralalbedosarehighlysensitivetothevegetationtypeandsolarzenithanglewhileBRDFatTOAdependsmoreonatmosphericconditionsandtheviewinggeometry.ComparisonwiththeCloudsandtheEarth'sRadiantEnergySystem(CERES)derivedclearskyAngularDistributionModel(ADM)forcropandgrassscenetypeshowsastandarddeviationof0.08inbroadbandanisotropicfunctionat25°solarzenithangleand0.15at50°solarzenithangle,respectively.
出版日期
2001年05月15日(中国期刊网平台首次上网日期,不代表论文的发表时间)