Single-scattering albedo
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Single-scattering albedo is the ratio of scattering efficiency to total extinction efficiency (which is also termed "attenuance", a sum of scattering and absorption). Most often it is defined for small-particle scattering of electromagnetic waves. Single-scattering albedo is unitless, and a value of unity implies that all particle extinction is due to scattering; conversely, a single-scattering albedo of zero implies that all extinction is due to absorption. For spherical particles one can calculate single-scattering albedo from Mie theory and knowledge of bulk properties of material such as
refractive index In optics, the refractive index (or refraction index) of an optical medium is a dimensionless number that gives the indication of the light bending ability of that medium. The refractive index determines how much the path of light is bent, ...
. For non-spherical particles one could use discrete dipole approximation or other methods of computational electromagnetics. The albedo of particles of shapes which are easily parameterized in non-standard co-ordinate systems may be determined through solutions of Maxwell's equation analogues in such coordinate systems. Scattering albedo equations have yet to be determined in elliptical, toroidal, conical and many others. Derivation and solutions to such equations is a field of ongoing research.


See also

* Light scattering by particles *
Albedo Albedo (; ) is the measure of the diffuse reflection of solar radiation out of the total solar radiation and measured on a scale from 0, corresponding to a black body that absorbs all incident radiation, to 1, corresponding to a body that refle ...


References

*H. C. van de Hulst: ''Light scattering by small particles'', New York, Dover, 1981. *C. F. Bohren, D. R. Huffmann: ''Absorption and scattering of light by small particles''. New York, Wiley-Interscience, 1983. Scattering, absorption and radiative transfer (optics) Atmospheric radiation Aerosol measurement {{astronomy-stub