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Mathematical model of solar radiation reflection by underlying surface

机译:下层表面太阳辐射反射的数学模型

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The model of a plane-parallel slab of a turbid medium is accepted, where there are particles of the spherical form scattering light separately from each other. Mathematically the problem is reduced to the solution of a boundary-value problem of a radiative transfer equation in turbid media with strong anisotropic scattering. In this case the computation of a backscattering is mathematically an ill-conditioned problem by using any numerical method of the solution. In the suggested method the backscattering radiance is determined by a SH method as a difference between the exact solution and SAA that essentially reduces the order of a system and smoothes the solution at any degree of an anisotropy scattering. As SAA the small angle modification of spherical harmonics method is chosen, which has a form of series of spherical harmonics that also enables to present a backscattering analytically. The calculation of medium parameters in model is made according to the Mie theory in the form of series of spherical harmonics, that allows to take into account the effect of physical properties of the medium on the radiation reflection.
机译:接受浑浊介质的平面平行平板的模型,其中存在球形的颗粒,它们彼此分开散射光。从数学上讲,该问题被简化为具有强各向异性散射的混浊介质中辐射传递方程的边值问题的解。在这种情况下,通过使用解的任何数值方法,反向散射的计算在数学上都是病态问题。在建议的方法中,后向散射辐射通过SH方法确定为精确解和SAA之间的差,该差实质上减小了系统阶数,并在任何程度的各向异性散射下使溶液平滑。作为SAA,选择了球谐函数的小角度修改方法,该方法具有一系列球谐函数的形式,这也使得能够解析地显示反向散射。模型中的介质参数的计算是根据Mie理论以一系列球谐函数的形式进行的,从而可以考虑介质的物理特性对辐射反射的影响。

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