An infralateral arc (or lower lateral tangent arc) is a rare halo, an
optical phenomenonappearing similar to a rainbowunder a white parhelic circle. Together with the supralateral arcthey are always located outside the seldom observable 46° halo, but in contrast to supralateral arcs, infralateral arcs are always located below the parhelic circle.
The shape of an infralateral arc varies with the elevation of the
sun. Between sunrise and before the sun reaches about 50° over the horizon, two infralateral arcs are located on either side (e.g. lateral) of the 46° halo, their convex apexes lying tangentto the 46° halo. As the sun reaches above 68° the two arcs unite to a single concave arc tangent to the 46° halo vertically under the sun.cite web
url = http://www.meteoros.de/arten/ee22e.htm
title = Infralateral arc | publisher = Arbeitskreis Meteore e.V.
accessdate = 07-04-16 | language = English (Including a photo from January 1996 and a 1980 computer simulation of infra- and supralateral arcs relative to a 46° halo.)]
Infralateral arcs form when sun light enters horizontally oriented, rod-shaped
hexagonal ice crystals through a hexagonal base and exits through one of the prism sides. Infralateral arcs occur about once a year. They are often observed together with circumscribed halos and upper tangent arcs.cite web
url = http://www.engl.paraselene.de/html/infralateral_arcs.html
title = Infralateral Arcs | publisher = www.paraselene.de
accessdate = 2007-04-16 | language = English]
* [http://www.atoptics.co.uk/halo/supinf.htm Atmospheric Optics - Supralateral & infralateral arcs] - including
HaloSimcomputer simulations and crystal illustrations.
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