| The circumzenithal arc, oft mistaken for a rainbow,  can be ephemeral.   Always close  to the zenith, the ice crystal cirrus clouds forming it scud across quickly, brightening  and then dimming the arc in seconds.
 It has the purest and brightest colours (with its  matching circumhorizon arc) of all the halos.
 
 Plate crystals generating it are aerodynamic drag aligned with their  large hexagonal faces usually within a degree or better of horizontal.   Nearly parallel sun rays stream into the  upper face and leave through a vertical side face.    Nature  creates an almost ideal laboratory spectrum demonstration where collimated  light shines through a clamped 90° prism.    Have dark Fraunhofer lines ever been observed in a CZA?
 
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