The Successive-Order-of-Interaction Radiative Transfer Model. Part I: Model Development
Open Access
- 1 October 2006
- journal article
- Published by American Meteorological Society in Journal of Applied Meteorology and Climatology
- Vol. 45 (10) , 1388-1402
Abstract
This study, the first part of a two-part series, develops the method of “successive orders of interaction” (SOI) for a computationally efficient and accurate solution for radiative transfer in the microwave spectral region. The SOI method is an iterative approximation to the traditional adding and doubling method for radiative transfer. Results indicate that the approximations made in the SOI method are accurate for atmospheric layers with scattering properties typical of those in the infrared and microwave regions. In addition, an acceleration technique is demonstrated that extends the applicability of the SOI approach to atmospheres with greater amounts of scattering. A comparison of the SOI model with a full Monte Carlo model using the atmospheric profiles given by Smith et al. was used to determine the optimal parameters for the simulation of microwave top-of-atmosphere radiances. This analysis indicated that a four-stream model with a maximum initial-layer optical thickness of approximately ... Abstract This study, the first part of a two-part series, develops the method of “successive orders of interaction” (SOI) for a computationally efficient and accurate solution for radiative transfer in the microwave spectral region. The SOI method is an iterative approximation to the traditional adding and doubling method for radiative transfer. Results indicate that the approximations made in the SOI method are accurate for atmospheric layers with scattering properties typical of those in the infrared and microwave regions. In addition, an acceleration technique is demonstrated that extends the applicability of the SOI approach to atmospheres with greater amounts of scattering. A comparison of the SOI model with a full Monte Carlo model using the atmospheric profiles given by Smith et al. was used to determine the optimal parameters for the simulation of microwave top-of-atmosphere radiances. This analysis indicated that a four-stream model with a maximum initial-layer optical thickness of approximately ...Keywords
This publication has 13 references indexed in Scilit:
- The Successive-Order-of-Interaction Radiative Transfer Model. Part II: Model Performance and ApplicationsJournal of Applied Meteorology and Climatology, 2006
- Fast Computation of Microwave Radiances for Data Assimilation Using the “Successive Order of Scattering” MethodJournal of Applied Meteorology and Climatology, 2005
- A fast multistream scattering-based Jacobian for microwave radiance assimilationIEEE Transactions on Geoscience and Remote Sensing, 2004
- Intercomparison of microwave radiative transfer models for precipitating cloudsIEEE Transactions on Geoscience and Remote Sensing, 2002
- A Microwave Polarimetric Two-Stream Radiative Transfer ModelJournal of the Atmospheric Sciences, 2002
- Comparison of the Gauss–Seidel spherical polarized radiative transfer code with other radiative transfer codesApplied Optics, 1995
- Physical retrievals of over-ocean rain rate from multichannel microwave imagery. Part I: Theoretical characteristics of normalized polarization and scattering indicesMeteorology and Atmospheric Physics, 1994
- Radiative transfer by doubling very thin layersThe Astrophysical Journal, 1969
- Matrix Methods for Multiple-Scattering ProblemsJournal of the Atmospheric Sciences, 1966
- Multiple Scattering by Large Particles.The Astrophysical Journal, 1965