circumzenithal arc [¦sǝr·kǝm¦zē·nǝ·thǝl `ärk] OPTICS A brilliant rainbow-colored arc of about a quarter of a circle with its center at the zenith and about 46° above the sun, produced by refraction and dispersion of the sun's light striking the top of prismatic ice crystals in the atmosphere, and usually lasting only a few minutes. |