Abstract
The solution of the generalized two‐stream approximation for radiative transfer in homogeneous multiple scattering atmospheres is extended to vertically inhomogeneous atmospheres in a manner which is numerically stable and computationally efficient. It is shown that solar energy deposition rates, photolysis rates, and infrared cooling rates all may be calculated with simple modifications of a single algorithm. The accuracy of the algorithm is generally better than 10% so that other uncertainties, such as in absorption coefficients, may often dominate the error in calculation of the quantities of interest to atmospheric studies.
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Publication Info
- Year
- 1989
- Type
- article
- Volume
- 94
- Issue
- D13
- Pages
- 16287-16301
- Citations
- 989
- Access
- Closed
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Identifiers
- DOI
- 10.1029/jd094id13p16287