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SOME EXACT SOLUTIONS FOR COUPLED ATMOSPHERE-SURFACE RADIATION MODELS

机译:耦合的大气-表面辐射模型的某些精确解

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摘要

The problem of a plane parallel atmosphere bounded below by a reflecting surface is considered. It is well known that when that surface reflects isotropically, the radiation distribution emerging from the top of the atmosphere may be expressed in terms of the scattering and transmission functions of that atmosphere. For more general non-Lambertian surfaces this is not usually the case. However, it will be shown that for a certain class of surfaces this can still be done, and the problem reduced to evaluating certain integrals; the integrands of which are the product of ground reflectance terms and either the scattering or transmission functions of the atmosphere. The models described in this note were derived in order to provide ''closed form'' solutions with which to validate coupled atmospheric-surface radiation code, but they have a certain intrinsic interest beyond that, and may find application in sensitivity studies of retrieval algorithms for data from multi-view satellite instruments. Copyright (C) 1996 Elsevier Science Ltd. [References: 13]
机译:考虑到平面平行大气在下面被反射表面所限制的问题。众所周知,当该表面各向同性地反射时,可以根据该大气的散射和透射函数来表达从大气顶部出现的辐射分布。对于更一般的非朗伯曲面,通常不是这种情况。然而,将表明,对于某些类别的曲面,仍然可以做到这一点,并且问题减少到评估某些积分;其积分是地面反射率项与大气的散射或透射函数的乘积。本说明中描述的模型是为了提供“闭合形式”的解决方案而派生出来的,可用来验证耦合的大气表面辐射代码,但除此之外,它们还有一定的内在兴趣,并可能在检索算法的敏感性研究中得到应用用于多视图卫星仪器的数据。版权所有(C)1996 Elsevier Science Ltd. [引用:13]

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