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・ Diamond Days (Out of the Grey album)
・ Diamond Days (The Outfield album)
・ Diamond Daze
・ Diamond Dick
・ Diamond Dixon
・ Diamond Dogs
・ Diamond Dogs (band)
・ Diamond Dogs (disambiguation)
・ Diamond Dogs (film)
・ Diamond Dogs (song)
・ Diamond Dogs Tour
・ Diamond Dogs, Turquoise Days
・ Diamond Donner
・ Diamond dove
・ Diamond Dove (novel)
Diamond dust
・ Diamond dust (disambiguation)
・ Diamond Elementary School
・ Diamond Energy
・ Diamond enhancement
・ Diamond Estates Wines & Spirits Ltd.
・ Diamond Exchange District
・ Diamond Executive Aviation
・ Diamond Eyes
・ Diamond Eyes (Boom-Lay Boom-Lay Boom)
・ Diamond Eyes (Deftones song)
・ Diamond Ferri
・ Diamond Fields Advertiser
・ Diamond Film
・ Diamond firetail


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Diamond dust : ウィキペディア英語版
Diamond dust

Diamond dust is a ground-level cloud composed of tiny ice crystals. This meteorological phenomenon is also referred to simply as ice crystals and is reported in the METAR code as IC. Diamond dust generally forms under otherwise clear or nearly clear skies, so it is sometimes referred to as clear-sky precipitation. It is most commonly observed in Antarctica and the Arctic, but it can occur anywhere with a temperature well below freezing. In polar regions diamond dust may continue for several days without interruption.
==Characteristics==

Diamond dust is similar to fog in that it is a cloud based at the surface; however, it differs from fog in two main ways. Generally fog refers to a cloud composed of liquid water (the term ice fog usually refers to a fog that formed as liquid water and then froze, and frequently seems to occur in valleys with airborne pollution such as Fairbanks, Alaska, while diamond dust forms directly as ice). Also, fog is a dense enough cloud to significantly reduce visibility, while diamond dust is usually very thin and may not have any effect on visibility (there are far fewer crystals in a volume of air than there are droplets in the same volume with fog). However, diamond dust can often reduce the visibility, in some cases to under .
The depth of the diamond dust layer can vary substantially from as little as to . Because diamond dust does not always reduce visibility it is often first noticed by the brief flashes caused when the tiny crystals, tumbling through the air, reflect sunlight to your eye. This glittering effect gives the phenomenon its name since it looks like many tiny diamonds are flashing in the air.

File:050207diamond dust1 Tsukuba Japan.png|Diamond dust briefly observed at Tsukuba, Japan. These are serial photos out of a movie; note differences in crystal locations.
File:050207diamond dust2 Tsukuba Japan.png|Temperature was -2 °C, relative humidity was almost 100%. These photos captured only the glittering particles.


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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