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Parry arc : ウィキペディア英語版
Parry arc

A Parry arc is a rare halo, an optical phenomenon which occasionally appears over a 22° halo together with an upper tangent arc.
== Discovery ==
The halo was first described by Sir William Edward Parry (1790–1855) in 1820 during one of his Arctic expeditions in search for the Northwest Passage. On April 8, under harsh conditions while his two ships were trapped by ice forcing him to winter over at Melville Island in the northern Canadian Arctic Archipelago, he made a drawing of the phenomenon. The drawing accurately renders the parhelic circle, a 22° halo, a pair of sun dogs, a lower tangent arc, a 46° halo, and a circumzenithal arc. He did, however, get the upper tangent arc slightly wrong. On the other hand, he added two arcs extending laterally from the bases of the 46° halo, for long interpreted as incorrectly drawn infralateral arcs, but, as thing were, probably correctly drawn subhelic arcs. (both produced by the same crystal orientation but with light passing through different faces of the crystals.)〔Cowley, ''Parry 1820''〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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