Anthelion

For the Taiwanese band, see Anthelion (band).

An anthelion (plural anthelia, from late Greek ανθηλιος, "opposite the sun") is a rare optical phenomenon appearing on the parhelic circle opposite to the sun as a faint white halo, not unlike a sundog.

Anthelion 120 parhelion depicted in Vädersolstavlan

How anthelions are formed is disputed. Walter Tape, among others, has argued they are not separate haloes, but simply where various haloes caused by horizontally oriented column-shaped ice crystals coincide on the parhelic circle to create a bright spot. If this theory is correct, anthelia should only appear together with these other haloes.[1]

However, anthelia occur unaccompanied by other plate crystal haloes, thus scientists have produced alternative explanations. The Dutch professor S.W. Visser proposed they form by two exterior light reflections in quadrangular prisms, while Robert Greenler has suggested two interior reflection in column-shaped crystals produces the phenomenon.[1]

While the anthelion area is usually sparse on haloes, in a complex display it features various rare optic phenomena: Flanking the anthelion on the parhelic circle are two 120° parhelia (and two Liljequist parhelia) caused by plate crystals. The Tricker and diffuse arcs are produced in singly oriented column crystals and form an Ankh-like shape passing through the anthelion. Wegener arcs occasionally crosses the sky to converge in the anthelion.[2]

See also

References

  1. 1 2 "Anthelion". Arbeitskreis Meteore e.V. Retrieved 2007-04-22.
  2. ↑ Les Cowley. "South Pole Halos - Anthelic View". Atmospheric Optics. Retrieved 2007-04-22. (including fish eye photo a.o.)

External links

Wikisource has the text of the 1911 Encyclopædia Britannica article Anthelion.


This article is issued from Wikipedia - version of the 11/16/2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.