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Antisolar point

From Wikipedia, the free encyclopedia
Point on the celestial sphere opposite Sun
Arainbow has 42° centered around the antisolar point, which always coincides with the shadow of the observer's eye/camera, seen here at the bottom of the frame.
Drawing byRené Descartes explaining the formation of arainbow. The antisolar point is the center of the rainbowM. It lies at the end of the straight line running from the sun through the observer's eyeE.
Centered on the antisolar point, this photo features various antisolar/subhorizonhaloes, as viewed from a plane.

Theantisolar point is theabstract point on thecelestial sphere directly opposite theSun from an observer'sperspective.[1] This means that the antisolar point lies above thehorizon when the Sun is below it, and vice versa. On asunny day, the antisolar point can be easily found; it is located within theshadow of the observer's head. Like thezenith andnadir, the antisolar point is not fixed inthree-dimensional space, but is defined relative to the observer. Each observer has an antisolar point that moves as the observer changes position.

The antisolar point forms thegeometric center of severaloptical phenomena, including subhorizonhaloes,rainbows,[2]glories,[3] theBrocken spectre, andheiligenschein. Occasionally, aroundsunset orsunrise,anticrepuscular rays appear to converge toward the antisolar point near the horizon.[4] However, this is anoptical illusion caused by perspective; in reality, the "rays" (i.e. bands of shadow) run near-parallel to each other.[5]

Also around the antisolar point, thegegenschein is often visible in a moonlessnight sky away fromcity lights, arising from thebackscatter ofsunlight byinterplanetary dust. Inastronomy, thefull Moon or aplanet inopposition lies near the antisolar point. During a totallunar eclipse, the full Moon enters theumbra ofEarth's shadow, which the planet casts ontoits atmosphere, into space, and toward the antisolar point.

Anthelic point

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Theanthelic point is often used as a synonym for the antisolar point, but the two should be differentiated.[1]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 elevation as the sun, and is therefore located on theparhelic circle. There are severalhalo phenomena that are centered on or converge on the anthelic point, such as theanthelion, Wegener arcs, Tricker arcs and the parhelic circle itself.[6][7][8]

See also

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References

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  1. ^abHerd, Tim (2007)."Angular Measurements in the sky".Kaleidoscope Sky. Abrams. p. 27.ISBN 081099397X.
  2. ^Cowley, Les."Primary rainbows". atoptics.co.uk. Retrieved13 September 2013.
  3. ^Cowley, Les."The Glory". atoptics.co.uk.
  4. ^Cowley, Les."Anticrepuscular rays". atoptics.co.uk. Retrieved13 September 2013.
  5. ^Cowley, Les."Antisolar or anticrepuscular rays". atoptics.co.uk.
  6. ^Alexander Wünsche; Jim Foster,Anthelion and anthelic arcs, 2006
  7. ^Walter Tape,Atmospheric Halos,ISSN 0066-4634,ISBN 0875908349, American Geophysical Union, 1994, p. 27
  8. ^Les Cowley.South Pole Halos – Anthelic View – Atmospheric OpticsArchived 2015-09-23 at theWayback Machine, accessed 13 September 2013
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