The matrix operator approach to radiative transfer is shown to be a very powerful technique in establishing symmetry relations for multiple scattering in inhomogeneous atmospheres. Symmetries are derived for the reflection and transmission operators using only the symmetry of the phase function. These results will mean large savings in computer time and storage for performing calculations for realistic planetary atmospheres using this method. The results have also been extended to establish a condition on the reflection matrix of a boundary in order to preserve reciprocity. Finally energy conservation is rigorously proven for conservative scattering in inhomogeneous atmospheres
AbstractIn this paper, we developed two methods to solve the inverse problem of a nonlinear integro-...
The complete radiation field including polarization is calculated for a model of the real atmosphere...
The polarization of electromagnetic radiation reflected by a particulate surface is determined by a ...
Entirely rigorous proofs of the symmetries induced by the phase matrix into the reflection and trans...
An entirely rigorous method for the solution of the equations for radiative transfer based on the ma...
The matrix operator method of solving radiation transfer problems is extended to include polarizatio...
The research accomplished during this period is briefly summarized. The interior radiances within an...
A mathematical justification is given for the multiple interface reflection expansion arising when u...
In this paper the general equations of transfer for an atmosphere scattering radiation in accordance...
We use Ambartsumian's method of addition of layers to show that various problems, including the stan...
This paper outlines the matrix exponential description of radiative transfer. The eigendecomposition...
The exact solutions are obtained for a one dimensional model of a scattering and absorbing medium. T...
The principal elements of the theory of polarized light transfer in planetary atmospheres are expoun...
In this paper the theory of diffuse reflection and transmission by a plane-parallel atmosphere of fi...
A theory of the multiple scattering of polarized light is discussed using the doubling method of van...
AbstractIn this paper, we developed two methods to solve the inverse problem of a nonlinear integro-...
The complete radiation field including polarization is calculated for a model of the real atmosphere...
The polarization of electromagnetic radiation reflected by a particulate surface is determined by a ...
Entirely rigorous proofs of the symmetries induced by the phase matrix into the reflection and trans...
An entirely rigorous method for the solution of the equations for radiative transfer based on the ma...
The matrix operator method of solving radiation transfer problems is extended to include polarizatio...
The research accomplished during this period is briefly summarized. The interior radiances within an...
A mathematical justification is given for the multiple interface reflection expansion arising when u...
In this paper the general equations of transfer for an atmosphere scattering radiation in accordance...
We use Ambartsumian's method of addition of layers to show that various problems, including the stan...
This paper outlines the matrix exponential description of radiative transfer. The eigendecomposition...
The exact solutions are obtained for a one dimensional model of a scattering and absorbing medium. T...
The principal elements of the theory of polarized light transfer in planetary atmospheres are expoun...
In this paper the theory of diffuse reflection and transmission by a plane-parallel atmosphere of fi...
A theory of the multiple scattering of polarized light is discussed using the doubling method of van...
AbstractIn this paper, we developed two methods to solve the inverse problem of a nonlinear integro-...
The complete radiation field including polarization is calculated for a model of the real atmosphere...
The polarization of electromagnetic radiation reflected by a particulate surface is determined by a ...