Bi-hemispherical reflectance

Bi-hemispherical reflectance is the reflectance of a surface under diffuse illumination (with no direct component). Bi-hemispherical reflectance is an important part of the Bidirectional reflectance distribution function over all viewing and illumination directions of a hemisphere.[1] It is sometimes called "white-sky albedo".

See also

References
  1. Nicodemus, F.E.; J.C. Richmond; J.J. Hsia (October 1977). Geometrical Considerations and Nomenclature for Reflectance (PDF). National Bureau of Standards. Bibcode:1977nbs..reptR....N. Retrieved 8 April 2013.


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.