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High-accuracy measurements of snow Bidirectional Reflectance Distribution Function at visible and NIR wavelengths – comparison with modelling results

机译:高精度测量雪在可见光和NIR波长的双向反射分布函数–与建模结果比较

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摘要

High-accuracy measurements of snow Bidirectional Reflectance DistributionFunction (BRDF) were performed for four natural snow samples with aspectrogonio-radiometer in the 500–2600 nm wavelength range. Thesemeasurements are one of the first sets of direct snow BRDF values over a widerange of lighting and viewing geometry. They were compared to BRDF calculatedwith two optical models. Variations of the snow anisotropy factor withlighting geometry, wavelength and snow physical properties were investigated.Results show that at wavelengths with small penetration depth, scatteringmainly occurs in the very top layers and the anisotropy factor is controlledby the phase function. In this condition, forward scattering peak or doublescattering peak is observed. In contrast at shorter wavelengths, thepenetration of the radiation is much deeper and the number of scatteringevents increases. The anisotropy factor is thus nearly constant and decreasesat grazing observation angles. The whole dataset is available on demand fromthe corresponding author.
机译:使用方面反射辐射计在500–2600 nm波长范围内对四个天然雪样本进行了雪的高精度双向反射分布函数(BRDF)测量。这些测量是在广泛的照明和观察几何条件下,第一批直接降雪BRDF值之一。将它们与使用两个光学模型计算的BRDF进行了比较。研究了雪各向异性因子随照明几何形状,波长和雪物理性质的变化。结果表明,在穿透深度较小的波长下,散射主要发生在最顶层,并且各向异性因子受相函数控制。在这种情况下,观察到前向散射峰或双散射峰。相反,在较短的波长下,辐射的穿透深度更大,并且散射事件的数量增加。因此,各向异性因子几乎恒定,并且在掠射观察角处减小。整个数据集可根据需要从相应的作者那里获得。

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