Transfer of solar irradiance through inhomogeneous turbid atmospheres evaluated by Eddington's approximation

Abstract

Eddington's approximation was employed to compute the irradiances passing through atmospheres consisting of several different, albeit internally homogeneous, layers, as a function of solar zenith angle, albedo for single scattering, the asymmetry factor of the phase function, and the albedo of the underlying surface. Results computed for a single layer atmosphere %were found to agree with more exact computations within a few percent. Irradiances within several vertically inhomogeneous three- layer model atmospheres were computed. Effects caused by the vertically inhomogeneous structure are considered.