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The circumzenithal arc or circumzenith arc (CZA), also called the Bravais' arc, is an optical phenomenon similar in appearance to a rainbow; but it arises from refraction of sunlight through horizontally-oriented ice crystals, generally in cirrus clouds, rather than from raindrops. It forms no more than one-quarter of a circle centered on the zenith and on the same side as the sun. Its colors are from blue on the inside to red on the outside of the arc. It is one of the brightest and most colorful halos. Its colors are purer than those of the rainbow because there is much less color overlap in its formation. The first impression is that of an upside-down rainbow. The circumzenithal arc has been called "a smile in the sky". It is rarely noticed because it occurs so far overhead, but in fact is relatively common.[citation needed] Cirrus clouds which cause a sun dog can cause a circumzenithal arc when they reach the zenith, if the Sun is low in the sky.
Originally posted by C.H.U.D.
reply to post by incrediblelousminds
Besides the circumzenithal ark, you also have a much rarer 46° halo in your photographs. Good catch
Originally posted by C.H.U.D.
You're welcome incrediblelousminds.
A single (the inner 22°) halo is actually quite common. I see them usually at least once or twice a week. The 46° (outer) halo which shows up best on your second shot, is much rarer. I've not seen one yet, but then I've only been looking out for halos and arcs for a couple of years now. Sometimes halos and arcs are very short lived, so catching a good display like yours takes a bit of luck and/or more time spent looking up.
It sounds like you have a good feel for the type of conditions (hazy high altitude cloud) that produce halos, so look more frequently when you see those conditions and you'll see lots more.