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单词 Circumzenithal arc
释义

Circumzenithal arc

中文百科

环天顶弧

位于美国麻萨诸塞州塞勒姆的环天顶弧,摄于2012年10月27日。影像中同时可见太阳上侧弧(Supralateral arc)、彩晕弧(Parry arc)和上正切晕弧(Upper tangent arc)。
摄于2005年7月10日。
2007年1月摄于美国北达科他州大福克斯。

环天顶弧英语:circumzenithal arccircumzenith arc,缩写:CZA)或称布拉维弧Bravais' arc),是一种在外观上类似彩虹的光学现象;但它的形成是太阳光从水平方向通过冰晶(一般位于卷云内)后折射而形成,而非雨滴。

英语百科

Circumzenithal arc 环天顶弧

Circumzenithal arc in Salem, Massachusetts, Oct 27, 2012. Also visible are a supralateral arc, Parry arc, and upper tangent arc.
摄于2005年7月10日。
2007年1月摄于美国北达科他州大福克斯。
Arc circumzénithal

The circumzenithal arc or circumzenith arc (CZA), also called the Bravais' arc, is an optical phenomenon similar in appearance to a rainbow, but it belongs to the family of halos arising from refraction of sunlight through ice crystals, generally in cirrus or cirrostratus clouds, rather than from raindrops. The arc is located at a considerable distance (approximately 46°) above the sun and at most forms a quarter of a circle centered on the zenith. It has been called "a smile in the sky", its first impression being that of an upside-down rainbow. The CZA is one of the brightest and most colorful members of the halo family. Its colors, ranging from violet on top to red at the bottom, are purer than those of a rainbow because there is much less overlap in their formation.

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