Parhelic circle


A parhelic circle is a 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.
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.
Parhelic circles form as beams of sunlight are reflected by vertical or almost vertical hexagonal ice crystals. The reflection can be either external which contributes to the parhelic circle near the sun, or internal 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. Sun dogs are always aligned to the parhelic circle.
The intensity distribution of the parhelic circle is largely dominated by 1-3-2 and 1-3-8-2 rays. The former ray-path is responsible for the blue spot halo which occurs at an azimuth.
with being the material's index of refraction. However, many more features give a structure to the intensity pattern of the parhelic circle. Among the features of the parhelic circle are the Liljequist parhelia, the 90° parhelia, the second order 90° parhelia, the 22° parhelia and more.
Artificial parhelic circles can be realized by experimental means using, for instance, spinning crystals.