© Claudia Hinz
Neklid, Klinovec, Czech Republic
Latitude: 50° 24' 12'' N
Longitude: 12° 56' 19'' E
30 January 2014 1056 (Local Time)
Camera direction: towards SSE
Image P/S code: P.13.1
Image I.D.: 4204
This magnificent halo display was formed by the refraction and reflection of sunlight through diamond dust at an altitude of 1 100 m in Neklid, Klinovec, Ore Mountains, Czech Republic.
Such complex displays are usually observed only in polar regions, although they may occasionally occur in mountains when there are ice crystals in the air, as in this case. The dust-like specks in this photograph are in fact the diamond dust ice crystals sparkling in the sunlight.
The halos visible in this picture are: a 22° halo; a parhelic circle and parhelia; a lower tangent arc; infralateral arcs; an upper tangent arc with a suncave Parry arc; a heliac arc; a supralateral arc that touches a circumzenithal arc; and four Tape arcs (also known as 46° Parry arcs).
Some of these halo types are quite common, such as the 22° halo and the parhelia. Others, however, are less frequently seen, and some, such as the heliac arc and Tape arcs, are rarely witnessed.
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Links in the image description will highlight features on the image. Mouse over the features for more detail.
Links in the image description will highlight features on the image. Mouse over the features for more detail.
The veil of Cirrostratus nebulosus is almost invisible and probably only a small height above the ice cap. The halo phenomena comprise two portions of a 22° halo at 1 and 2 and left and right parhelia at 3 and 4, presumably with arcs of Lowitz. There is also a vague indication of a cross at 5 - 6, 7 - 8.
The place of observation was in a flow of maritime polar air from the south.
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