Two-stream approximation

From Wikipedia, the free encyclopedia

In models of radiative transfer, the two-stream approximation is a discrete ordinate approximation in which radiation propagating along only two discrete directions is considered. It was first used by Arthur Schuster in 1905.[1] The two ordinates are chosen such that the model captures the essence of radiative transport in light scattering atmospheres.[2] A practical benefit of the approach is that it reduces the computational cost of integrating the radiative transfer equation. The two-stream approximation is commonly used in parameterizations of radiative transport in global circulation models and in weather forecasting models, such as the WRF. There is a large number of applications of the two-stream approximation, including variants such as the . It is the simplest approximation that can be used to explain common observations inexplicable by single-scattering arguments, such as the brightness and color of the clear sky, the brightness of clouds, the whiteness of a glass of milk, and the darkening of sand upon wetting.[3] The two-stream approximation comes in many variants, including the Eddington approximation, as well as the modified Eddington, Quadrature, and Hemispheric constant models.[2] Mathematical descriptions of the two-stream approximation are given in several books.[4][5]

See also[]

  • List of atmospheric radiative transfer codes

Notes and references[]

  1. ^ Liou, K. N. (2002-05-09). An Introduction to Atmospheric Radiation. p. 106. ISBN 9780080491677. Retrieved 2017-10-22.
  2. ^ a b W.E. Meador and W.R. Weaver, 1980, Two-Stream Approximations to Radiative Transfer in Planetary Atmospheres: A Unified Description of Existing Methods and a New Improvement, 37, Journal of the Atmospheric Sciences, 630–643 http://journals.ametsoc.org/doi/pdf/10.1175/1520-0469%281980%29037%3C0630%3ATSATRT%3E2.0.CO%3B2
  3. ^ Bohren, Craig F., 1987, Multiple scattering of light and some of its observable consequences, American Journal of Physics, 55, 524-533.
  4. ^ G. E. Thomas and K. Stamnes (1999). Radiative Transfer in the Atmosphere and Ocean. Cambridge University Press. ISBN 0-521-40124-0.
  5. ^ Grant W. Petty (2006). A First Course In Atmospheric Radiation (2nd Ed.). Sundog Publishing, Madison, Wisconsin. ISBN 0-9729033-0-5.
Retrieved from ""