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Theoretical study of solar light reflectance from vertical snow surfaces

机译:垂直积雪表面太阳光反射率的理论研究

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The influence of horizontal and vertical inhomogeneity of snow surfaces onsolar light reflectance is studied using the radiative transfer theory (RTT).We compared 1-D RTT and 2-D RTT and found that large errors are produced ifthe 1-D RTT is used for the calculation of the snow reflection function (and,therefore, also in the retrievals of the snow grain radii) in 2-D measurementgeometries. Such 2-D geometries are common in the procedures for thedetermination of the effective snow grain radii using near-infraredphotography and spectroscopy of vertical snow walls. In particular, we haveconsidered three cases for the numerical calculations: (1) the case with noblack film; (2) the case with a black film at the pit's bottom; (3) the casewith a black film at the pit's bottom and also at one of the vertical snowwalls.
机译:利用辐射传输理论(RTT)研究了雪面水平和垂直不均匀性对太阳光反射率的影响,我们比较了1-D RTT和2-D RTT,发现使用1-D RTT会产生较大的误差。二维测量几何中的积雪反射函数的计算(因此也包含在积雪半径的检索中)。在使用近红外照相法和垂直雪壁的光谱法确定有效雪粒半径的过程中,这种二维几何结构很常见。特别是,我们考虑了三种情况进行数值计算:(1)没有黑膜的情况; (2)坑底有黑膜的情况; (3)在底坑的底部以及其中一个垂直雪壁处有黑色薄膜的情况。

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