Earth:Parhelic circle
Photo: Cindy McFee, NOAA, December 1980.[1]
A parhelic circle is a type of halo, an optical phenomenon appearing as a horizontal white line on the same altitude as the Sun, or occasionally the Moon. If complete, it stretches all around the sky, but more commonly it only appears in sections.[2] If the halo occurs due to light from the Moon rather than the Sun, it is known as a paraselenic circle.[3]
Even fractions of parhelic circles are less common than sun dogs and 22° halos. While parhelic circles are generally white in colour because they are produced by reflection, they can however show a bluish or greenish tone near the 120° parhelia and be reddish or deep violet along the fringes.[4]
Parhelic circles form as beams of sunlight are reflected by vertical or almost vertical hexagonal ice crystals. The reflection can be either external (e.g. without the light passing through the crystal) which contributes to the parhelic circle near the Sun, or internal (one or more reflections inside the crystal) which creates much of the circle away from the Sun. Because an increasing number of reflections makes refraction asymmetric some colour separation occurs away from the Sun.[5] Sun dogs are always aligned to the parhelic circle (but not always to the 22° halo).[citation needed]
The intensity distribution of the parhelic circle is largely dominated by 1-3-2 and 1-3-8-2 rays (cf. the nomenclature by W. Tape, i.e. 1 denotes the top hexagonal face, 2 the bottom face, and 3-8 enumerate the side faces in counter-clockwise fashion. A ray is notated by the sequence in which it encounters the prism faces). The former ray-path is responsible for the blue spot halo which occurs at an azimuth.[6]
[math]\displaystyle{ \theta_{\mathfrak{1}\mathfrak{3}\mathfrak{2}}=2\arcsin\left(n\cos\left(\arcsin\left(1/n\right)\right)/\cos\left(e\right)\right) }[/math],
with [math]\displaystyle{ n }[/math] being the material's index of refraction (not the Bravais index of refraction for inclined rays). However, many more features give a structure to the intensity pattern of the parhelic circle.[7][8] Among the features of the parhelic circle are the Liljequist parhelia, the 90° parhelia (likely unobservable), the second order 90° parhelia (unobservable), the 22° parhelia and more.
Artificial parhelic circles can be realized by experimental means using, for instance, spinning crystals.
See also
References
- ↑ "A magnificent halo". NOAA. 1980-12-21. Archived from the original on 2006-12-13. https://web.archive.org/web/20061213123117/http://www.photolib.noaa.gov/historic/nws/wea00195.htm. Retrieved 2007-04-14.
- ↑ Koby Harati. "Parhelic Circle". Atmospheric Optics. http://www.atoptics.co.uk/halo/parcirc.htm. Retrieved 2007-04-15.
- ↑ Les Cowley. "Paraselenae & Paraselenic circle". Atmospheric Optics. https://www.atoptics.co.uk/fza40.htm. Retrieved 2021-10-07.
- ↑ "Parhelic Circle". www.paraselene.de. http://www.paraselene.de?uk:113554. Retrieved 2009-02-01. (including an excellent HaloSim simulation of a parhelic circle.)
- ↑ Les Cowley. "Parhelic Circle Formation". Atmospheric Optics. http://www.atoptics.co.uk/halo/pcpaths.htm. Retrieved 2007-04-15.
- ↑ Sillanpää, M.; Moilanen, J.; Riikonen, M.; Pekkola, M. (2001). "Blue spot on the parhelic circle". Applied Optics 40 (30): 5275–5279. doi:10.1364/ao.40.005275. PMID 18364808. Bibcode: 2001ApOpt..40.5275S.
- ↑ Selmke, M. (2015). "Artificial Halos". American Journal of Physics 83 (9): 751–760. doi:10.1119/1.4923458. Bibcode: 2015AmJPh..83..751S. http://scitation.aip.org/content/aapt/journal/ajp/83/9/10.1119/1.4923458.
- ↑ Borchardt, S.; Selmke, M. (2015). "Intensity distribution of the parhelic circle and embedded parhelia at zero solar elevation: theory and experiments". Applied Optics 54 (22): 6608–6615. doi:10.1364/AO.54.006608. PMID 26368071. Bibcode: 2015ApOpt..54.6608B. https://www.osapublishing.org/ao/abstract.cfm?uri=ao-54-22-6608.
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