Science. 1974 Dec 13;186(4168):1034-6. doi: 10.1126/science.186.4168.1034.
The ratio of the absorption coefficient to the backscatter coefficient for which heating and cooling effects due to aerosols exactly balance at the earth's surface has been calculated with the use of a radiative-convective atmospheric model. The results are compared with those obtained from several simpler mean radiative-transfer models.
利用辐射-对流大气模型计算了气溶胶在地球表面引起的加热和冷却效应精确平衡时的吸收系数与后向散射系数之比。并将结果与几个更简单的平均辐射传输模型的结果进行了比较。