Abstract
With the aid of computer-simulated halo patterns, we show that
Kern’s arc, as seen on the latitude of the circumzenithal arc and on
the other side of the zenith, is produced by double-plate ice crystals with a
vertical principal axis. Light rays that contribute to Kern’s arc are
demonstrated by geometric ray tracing. We also discuss the condition under
which an arc that is opposite a circumhorizontal arc can appear.
© 1997 Optical Society of America
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