摘要
Employing the strong fluctuation theory, the radiative transfer equation for strongly fluctuating, continuous random media; and the associated phase matrix and scattering coefficient are obtained. By using the Gaussian quadrature and the eigenvalue-eigenvector approaches, the vector thermal radiative transfer equation for a layer of random medium is solved and is favorably matched with the experimental data of snowfield in remote sensing. The comparison with the conventional theory for weak fluctuation is discussed.
Employing the strong fluctuation theory, the radiative transfer equation for strongly fluctuating, continuous random media; and the associated phase matrix and scattering coefficient are obtained. By using the Gaussian quadrature and the eigenvalue-eigenvector approaches, the vector thermal radiative transfer equation for a layer of random medium is solved and is favorably matched with the experimental data of snowfield in remote sensing. The comparison with the conventional theory for weak fluctuation is discussed.
基金
Project supported by the National Natural Science Foundation of China and the Fok Ying Tung Education Foundation.
