Crepuscular rays

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Crepuscular rays over Plymouth Sound, UK
Crepuscular rays as seen from space, illustrating their parallel nature

Crepuscular rays /krɪˈpʌskjʊlər/ (more commonly known as sunbeams, sun rays, splintered light, or god rays), in atmospheric optics, are rays of sunlight that appear to radiate from the point in the sky where the Sun is located. Shining through openings in clouds (particularly stratocumulus) or between other objects, these columns of sunlit particulates are separated by darker cloud-shadowed volumes. Despite seeming to converge toward the light source, the rays are in fact near-parallel shafts of sunlight. Their apparent convergence is a perspective effect. This phenomenon mimics the way parallel railway lines or long hallways, for example, seem to seek convergence at a distant vanishing point. The sun rays do converge toward the sun, but the sun is much farther away than the rays might suggest.[1][2][3]


The name comes from their frequent occurrences during twilight hours (those around dawn and dusk), when the contrasts between light and dark are the most obvious. Crepuscular comes from the Latin word "crepusculum", meaning twilight.[4]

Anticrepuscular rays[edit]

Anticrepuscular rays opposite the setting sun off the Florida Gulf Coast of the United States

The rays in some cases may extend across the sky and appear to converge at the antisolar point, the point on the sky sphere directly opposite the sun. In this case they are called anticrepuscular or antisolar rays.[5] These are not as easily spotted as crepuscular rays. This apparent dual convergence (to both the solar and antisolar points) is a perspective effect analogous to railway tracks appearing to converge to opposite points in opposite directions.[6]


Crepuscular Rays Reno Nevada USA during a sunset

Crepuscular rays usually appear orange because the path through the atmosphere at sunrise and sunset passes through up to 40 times as much air as rays from a high midday sun. Particles in the air scatter short wavelength light (blue and green) through Rayleigh scattering much more strongly than longer wavelength yellow and red light.

Alternative names[edit]

See also[edit]


  1. ^ "Crepuscular Rays". Weather World 2010. University of Illinois, Champaign-Urbana.
  2. ^ Schaefer, Vincent J.; Day, John A.; Pasachoff, Jay (1998). A Field Guide to the Atmosphere. Houghton Mifflin Harcourt. p. 169.
  3. ^ "Crepuscular Rays, India". Earth Observatory. NASA. Retrieved 2018-05-07.
  4. ^ Edens, Harald. "Crepuscular rays". Weather Photography lightning, clouds, atmospheric optics & astronomy. Retrieved November 1, 2011.
  5. ^ Cowley, Les. "Anti-solar (anti-crepuscular) rays". Atmospheric Optics. Retrieved March 19, 2015.
  6. ^ Day, John A. (2005). The Book of Clouds. Sterling. pp. 124–127. ISBN 978-1-4027-2813-6. Retrieved 2010-10-09.
  7. ^ a b "Light Shafts". Unreal Engine 4 Documentation. Archived from the original on 2018-11-17. Retrieved 2018-11-17.
  8. ^ E.g. this term is mentioned in: Krüger, Jens; Bürger, Kai; Westermann, Rüdiger (2006). "Interactive screen-space accurate photon tracing on GPUs" (PDF). Proceedings of the 17th Eurographics conference on Rendering Techniques (EGSR'06).

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