Radiative Transfer In An Atmosphere-Ocean System: A Matrix Operator Approach
Radiative Transfer In An Atmosphere-Ocean System: A Matrix Operator Approach
复制标题
大气-海洋系统中的辐射传输：矩阵算子方法
DOI：
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发表时间：
1978
期刊：
影响因子：
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通讯作者：
G. Plass
中科院分区：
文献类型：
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作者：
G. Kattawar;T. J. Humphreys;G. Plass
本文的目的是演示如何有效地实现矩阵算符方法来耦合大气和海洋的辐射场。给出了总光学厚度为τmax=10 0 0的保守瑞利散射介质的方位向平均辐射和辐照度随光学厚度的变化关系，其中介质界面的光学厚度分别为0.0 1、0.1、1.0和10.0，并具有不同的太阳入射角度。
It is the purpose of this paper to demonstrate how the matrix operator method can be effectively implemented to couple the radiation fields of the atmosphere and ocean. Azimuthally averaged radiances and irradiances are presented as a function of optical depth for a conservative Rayleigh scattering medium of total optical thickness τmax = 1000 with a dielectric interface placed at optical depths of 0.01, 0.1, 1.0, and 10.0, and for various solar incident angles.