• Source: Sunbeam

A sunbeam, in meteorological optics, is a beam of sunlight that appears to radiate from the position of the Sun. Shining through openings in clouds or between other objects such as mountains and buildings, these beams of particle-scattered sunlight are essentially parallel shafts separated by darker shadowed volumes. Their apparent convergence in the sky is a visual illusion from linear perspective. The same illusion causes the apparent convergence of parallel lines on a long straight road or hallway at a distant vanishing point. The scattering particles that make sunlight visible may be air molecules or particulates.




Crepuscular rays




Crepuscular rays or god rays are sunbeams that originate when the sun is just below the horizon, during twilight hours. Crepuscular rays are noticeable when the contrast between light and dark is most obvious. Crepuscular comes from the Latin word "crepusculum", meaning twilight. 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.
Loosely, the term "crepuscular rays" is sometimes extended to the general phenomenon of rays of sunlight that appear to converge at a point in the sky, irrespective of time of day.




Anticrepuscular rays



In some cases, sunbeams may extend across the sky and appear to converge at the antisolar point, the point on the celestial sphere opposite of the Sun's direction. In this case, they are called antisolar rays (anytime not during astronomical night) or anticrepuscular rays (during the twilight period). This apparent dual convergence (at both the solar and the antisolar points) is a perspective effect analogous to the apparent dual convergence of the parallel lines of a long straight road or hallway at directly opposite points (to an observer above the ground).




Alternative names






See also


Airglow – Faint emission of light by a planetary atmosphere
Anticrepuscular rays – Meteorological optical phenomenon
Light beam – Projection of light energy
Earth's shadow – Shadow that Earth itself casts through its atmosphere and into outer space
Rayleigh scattering – Light scattering by small particles
Sunlight – Light emitted by the Sun
Tyndall effect – Scattering of light by tiny particles in a colloidal suspension
Volumetric lighting – Effect in computer graphics




References






External links



Sunrays – Crepuscular rays, Explanation & Images
Detailed description of how crepuscular rays occur

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