Zirkumzenitalbogen (EE11)

Description

EE11 - Light Path
E11 - Circumzenithal Arc
Crystal type:
  • Plate crystals
Orientation:
  • Base horizontal
Path of light:
  • Refraction at upper base and one side face
Occurrence:
  • frequent (20-30 days per year)
The circumzenithal arc (abbr. CZA) is one of the most beautiful and colorful halo phenomena. Its coloration and brightness can match, or even surpass, the rainbow. Thus, it has often been mistaken for a rainbow. Unlike the rainbow, which forms a circle around the sun's antipoint, the circumzenithal arc is an arc around the zenith, with only the part facing the sun visible. Normally about a quarter of a circular arc is visible, in exceptional cases a semicircle. Its apex lies at about 48° above the sun. At a solar height of 32°, the circumzenithal arc disappears at the zenith. When the solar height is over 32°, it can no longer form. The circumzenithal arc reaches its greatest brightness at a solar position of 22.1°. Therefore, it is most often seen at a solar position between 15° and 25°.

Simulation

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Origin

The circumzenithal arc is formed just like the sun dogs on horizontally floating ice plates. Here, however, the light enters at the base surface of the plate and exits at a side surface. Since the side surfaces are perpendicular to the base surface, the refraction angle is 90°. If sun dogs are visible, there is a high probability, especially when the sun is between 15° and 25° high, that the circumzenithal arc can also be seen. Unfortunately, the circumzenithal arc is hardly known to anyone, even though it occurs almost as frequently as the rainbow. The main reason for this is probably that one has to look almost straight up to see it.

Photos

Circumzenithal Arc
Circumzenithal arc taken in Bamberg (Photo: Wolfgang Hinz)
Circumzenithal Arc at the Moon
Circumzenithal Arc at the Moon on 19.09.2013 (Photo: Hermann Koberger)
Circumzenithal Arc in the Bavarian Forest
Circumzenithal Arc in the Bavarian Forest, taken on 01.12.2012 (Photo: Stefan Engl)

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