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dc.contributor.authorStamnes, Knut
dc.date.accessioned2024-10-08T00:36:38Z
dc.date.available2024-10-08T00:36:38Z
dc.date.issued1980-04
dc.identifier.urihttp://hdl.handle.net/11122/15451
dc.descriptionUAG R-272, Scientific Reporten_US
dc.description.abstractThe difficulties inherent in the conventional numerical implementation of the discrete ordinate method (following Chandrasekhar’s prescription) for solving the radiative transfer equation are discussed. A matrix formulation is developed to overcome these difficulties, and it is specifically shown that the order of the algebraic eigenvalue problem can be reduced by a factor of 2. This results in considerable reduction of computing time, especially if high-order discrete ordinate solutions are desired. A new expression for the source function is derived and used to obtain angular distributions. By appealing to the reciprocity principle it is shown that substantial computational shortcuts are possible if only integrated quantities such as albedo and transmissivity are required. Comparison of fluxes calculated by the present approach with those obtained by other methods shows that low-order discrete ordinate approximations yield very accurate results. Thus, the present approach offers an efficient and reliable computational scheme that lends itself readily to the solution of a variety of radiative transfer problems in realistic planetary atmospheres.en_US
dc.description.sponsorshipThis research was supported by the National Science Foundation through grant ATM 76-17409 to the University of Alaska.en_US
dc.description.tableofcontentsAbstract – 1. Introduction – 2. The equation of radiative transfer – 3. Critique of previous numerical procedures – 4. Direct matrix solution – 5. Boundary conditions - a. General – b. Parallel incident beam – c. Reflection and transmission – 6. Source function and angular distribution – a. Homogeneous case – b. Inhomogeneous case – c. Parallel incident beam – 7. Simplified reflection and transmission calculations – a. The standard problem – b. The planetary problem – 8. Results and comparisons – a. Comparison with Liou’s (1973) computations – b. Comparison with other established methods – c. Rayleigh scattering—comparison with Dave and Canosa (1974) – d. Comparison with Wiscombe (1977) - e. Spherical albedo for a semi-infinite atmosphere—comparison with Dlugach and Yanovitskij (1974) – 9. Conclusion – Acknowledgments – References.en_US
dc.language.isoen_USen_US
dc.publisherGeophysical Institute at the University of Alaska Fairbanksen_US
dc.subjectScattering (Physics)en_US
dc.subjectAtmospheric radiationen_US
dc.subjectRadiative transferen_US
dc.titleOn the discrete ordinate method for radiative transfer calculations in anisotropically scattering atmospheresen_US
dc.typeReporten_US
refterms.dateFOA2024-10-08T00:36:40Z


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