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SURFACE CORRECTIONS FOR REMOTE SENSING REFLECTANCE IN CASE 2 WATERS OF LAKE SUPERIOR*

机译:遥感反射率的表面矫正,在湖泊湖中的2个水域*

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We establish the average wavelength dependence for rough-surface reflectance Srs(λ) in Lake Superior and determine its magnitude at any individual site by extrapolating the total reflectance RrsT(λ) at the site to the asymptotic limit of zero scattering where Srs≌RrsT. The results show that Srs(λ) differs from the flat-surface Fresnel reflectance used in standard calculations of the remote sensing reflectance Rrs(λ) attributed to scattering by particles and molecules in bulk water. Finding Srs(λ) is essential in accurate estimates of Rrs(λ) at ground truth stations used in calibration of satellite data for waters where the presence of colored dissolved organic matter (CDOM) often leads to negative values for Rrs if we assume Fresnel reflectance. We examine the differences between Fresnel reflectance and Srs and estimate the threshold concentration of CDOM that could produce negative values of Rrs if those differences are not taken into account in the calculation of Rrs.
机译:我们通过将位点的总反射率RRST(λ)推断到SRS≌RST的零散射的渐近极限将站点推断到零散射的渐近极限,建立苏必利湖粗糙表面反射率SRS(λ)的平均波长依赖性并在任何单独部位确定其幅度。结果表明,Srs(λ)与标准计算的平坦表面菲涅耳反射率不同,所述遥感反射率RRS(λ)的标准计算归因于粒子和分子在散装水中的分散。寻找SRS(λ)对于用于校准卫星数据的地面真理站的RRS(λ)的准确估计是必不可少的用于卫星数据的卫星数据,其中有色溶解有机物(CDom)的存在通常会导致RRS的负值,如果我们假设菲涅耳反射率。我们检查菲涅耳反射率和Srs之间的差异,并估计如果在计算RRS的计算中,如果没有考虑这些差异,则可以产生RRS的负值的CDOM的阈值浓度。

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