Jacqueline Lenoble, editor. Radiative Trasfer m 3'cattermg ad Absorbing Atmospheres: dard Computatioal Procedures. Studies in Geophysical Optics and Remote Sensing. A. Deepak, Hampton, Virginia, 1985.  Home/Search   Document Not in Database   Summary   Related Articles

....used in computer graphics [19] The successive kernels, or terms of the expansion, correspond to rays that have undergone increasing numbers of reflections. This very natural physical interpretation is often referred to as successive orders of scattering in radiative transfer literature [24, 38]. The method of discrete ordinates used in radiative heat tanslet [11, 23] atmospheric scattering [24] and neutron transport [7] works by applying quadrature rules to discretely sampled positions and directions. Thus, it is essentially an application of the Nystr;3m method. A major advantage of ....

....rays that have undergone increasing numbers of reflections. This very natural physical interpretation is often referred to as successive orders of scattering in radiative transfer literature [24, 38] The method of discrete ordinates used in radiative heat tanslet [11, 23] atmospheric scattering [24], and neutron transport [7] works by applying quadrature rules to discretely sampled positions and directions. Thus, it is essentially an application of the Nystr;3m method. A major advantage of the Nystom method is that it can easily accomodate differential operators by means of finite difference ....

Jacqueline Lenoble, editor. Radiative Trasfer m 3'cattermg ad Absorbing Atmospheres: dard Computatioal Procedures. Studies in Geophysical Optics and Remote Sensing. A. Deepak, Hampton, Virginia, 1985.

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