November - fog You are here: Home Photo gallery Atmospheric optics Ice crystal halos Circumzenith arc


The circumzenith arc is caused by sunlight being refracted by ice-crystal plates floating horizontally in the atmosphere. The light enters the top face of the plate and exits a sideface. As the crystals have freedom of rotation along their vertical axis, an arc is produced with constant elevation, thus a part of a circle with the zenith at its centre. Only the quarter circle towards the sun is visible. In rare cases, the circle has a larger extend, and in extremely rare cases, it may be completed by an arc on its other side, being referred to as Kern's arc.

3 photos in gallery
Click images for large photos




w-079-03

w-033-24

w-029-13