Occasionally, during sunset or sunrise, anticrepuscular rays can be seen to converge at the antisolar point. Also, on a moonless night away from city lights, it is often possible to see the gegenschein at that point, arising from the back-scattering of light by interplanetary dust. In astronomy, when the moon or planets are in opposition, they are found close to the antisolar point. The antisolar point is the center of rainbows, and can be easily found on a sunny day: it is located at the shadow of one's head.
The anthelic point is often used as a synonym for the antisolar point, but the two should be differentiated. While the antisolar point is directly opposite the sun, always below the horizon when the sun is up, the anthelic point is opposite but at the same altitude as the sun, and is therefore located on the parhelic circle. There are several halo phenomena that are centered on or converge on the anthelic point, such as the anthelion, Wegener arcs, Tricker arcs and the parhelic circle itself.
Notes and references
- Tim Herd. Angular Measurements in the sky, excerpt from Kaleidoscope Sky, page 27. ISBN 0-8109-9397-X, Abrams, 2007
- Les Cowley. Anticrepuscular rays, accessed 13 September 2013.
- Les Cowley. Primary rainbows - Atmospheric Optics, accessed 13 September 2013.
- Alexander Wünsche; Jim Foster, Anthelion and anthelic arcs, 2006
- Walter Tape, Atmospheric Halos, ISSN 0066-4634, ISBN 0875908349, American Geophysical Union, 1994, p. 27
- Les Cowley. South Pole Halos - Anthelic View - Atmospheric Optics, accessed 13 September 2013