Atmospheric optics ray-tracing codes

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Atmospheric optics ray tracing codes - this article list codes for light scattering using ray-tracing technique to study atmospheric optics phenomena such as rainbows and halos. Such particles can be large raindrops or hexagonal ice crystals. Such codes are one of many approaches to calculations of light scattering by particles.

Geometric optics (ray tracing)[edit]

Main article: Geometric optics

Ray tracing techniques can be applied to study light scattering by spherical and non-spherical particles under the condition that the size of a particle is much larger than the wavelength of light. The light can be considered as collection of separate rays with width of rays much larger than the wavelength but smaller than a particle. Rays hitting the particle undergoes reflection, refraction and diffraction. These rays exit in various directions with different amplitudes and phases. Such ray tracing techniques are used to describe optical phenomena such as rainbow of halo on hexagonal ice crystals for large particles. Review of several mathematical techniques is provided in series of publications.

The 46° halo was first explained as being caused by refractions through ice crystals in 1679 by the French physicist Edmé Mariotte (1620–1684) in terms of light refraction [1] Jacobowitz in 1971 was the first to apply the ray-tracing technique to hexagonal ice crystal. Wendling et al. (1979) extended Jacobowitz's work from hexagonal ice particle with infinite length to finite length and combined Monte Carlo technique to the ray-tracing simulations. [2] [3] [4]

Classification[edit]

The compilation contains information about the electromagnetic scattering by hexagonal ice crystals, large raindrops, and relevant links and applications.

Codes for light scattering by hexagonal ice crystals[edit]

Year Name Authors References Language Short Description
Halosim Les Cowley and Michael Schroeder Atmospheric Optics site

graphical user interface

It creates simulations by accurately tracing up to several million light rays through mathematical models of ice crystals.
2010 Halopoint2 Jukka Ruoskanen webpage

graphical user interface

Ray-tracing code for various ice crystals with graphical user interface
2008 HALOSKY [5] Stanley David Gedzelman source codes Ray-tracing codes for light scattering by hexagonal ice crystals.
1996 Ray tracing [6] Andreas Macke source codes Fortran 77 and Fortran99 Ray-tracing codes for light scattering by polyhedral shaped ice crystals.

Relevant scattering codes[edit]

External links[edit]

See also[edit]

References[edit]

  1. ^ E. Mariotte, Quatrieme Essay. De la Nature des Couleur (Paris, France: Estienne Michallet, 1681). Sun dogs as well as the 22° and 46° halos are explained in terms of refractions from ice crystals on pages 466 - 524.
  2. ^ Greenler, R. Rainbows, halos, and glories. Cambridge University Press, Cambridge, 1980.
  3. ^ Pattloch, F., and Trankle, E. ¨Monte carlo simulation and analysis of halo phenomena. J. Opt. Soc. Am 1, 5 (1984), 520–526.
  4. ^ A Study on Atmospheric Halo Visualization, Sung Min Hong and Gladimir Baranoski, Technical Report CS-2003-26 September, 2003, School of Computer Science, University of Waterloo, 200 University venue West Waterloo, Ontario, Canada N2L 3G1
  5. ^ Simulating halos and coronas in their atmospheric environment, Stanley David Gedzelman, Applied Optics, H158-H156.
  6. ^ Single Scattering Properties of Atmospheric Ice Crystals, Andreas Macke, Johannes Mueller, and Ehrhard Raschke, Journal of the Atmospheric Sciences, 1996, 2813-2825.