Halo (optical phenomenon)
A halo (unicode|ἅλως; also known as a nimbus, icebow or Gloriole) is an
optical phenomenonthat appears near or around the Sunor Moon, and sometimes near other strong light sources such as street lights. There are many types of optical halos, but they are mostly caused by ice crystals in cold cirrus clouds located high (5–10 km, or 3–6 miles) in the upper troposphere. The particular shape and orientation of the crystals is responsible for the type of halo observed. Lightis reflected and refracted by the ice crystalsand may split up into colors because of dispersion, similarly to the rainbow.
Sometimes in very cold weather optical halos are formed by crystals close to ground level, called
diamond dust. The crystals behave like jewels, refracting and reflecting sunlight between their faces, sending shafts of light in particular directions.
Atmospheric phenomena such as halos were used as an
empiricalmeans of weather forecastingbefore meteorologywas developed.
A light pillar, or sun pillar, appears as a vertical pillar or column of light rising from the sun near sunset or sunrise, though it can appear below the sun, particularly if the observer is at a high elevation or altitude. Hexagonal plate- and column-shaped ice crystals cause the phenomenon. Plate crystals generally cause pillars only when the sun is within 6 degrees of the horizon, or below it; column crystals can cause a pillar when the sun is as high as 20 degrees above the horizon. The crystals tend to orient themselves near-horizontally as they fall or float through the air, and the width and visibility of a sun pillar depends on crystal alignment.
Light pillars can also form around the moon, and around street lights or other bright lights. Pillars forming from ground-based light sources may appear much taller than those associated with the sun or moon. Since the observer is closer to the light source, crystal orientation matters less in the formation of these pillars.
An icebow is phenomenon similar to a
rainbowexcept that it is formed by the refractionof sunlight through cloud suspended ice crystals as opposed to raindrops or other liquid water suspended in the air. Generally the appearance is as arc sections as opposed to a full circle. Brighter sections usually occur above, below, and to the center (where the sun is visible). These bright areas are referred to as " sun dogs," "parhelia" (plural), or mock suns because of their bright appearance and possible confusion with the actual location of the sun. Those icebows that are caused by very small ice crystals are one colour, because diffractionblurs the colours together. A 22 degree icebow has red on the inside and blue on the outside.
diffractiondisc or Airy dischas similar appearance, but is a disk, rather than a ring, and has a red border on the inside. Its size depends on the size of the ice or water particles that cause it. These are also known as coronas, but are not to be confused with the thin streaming luminous gas that makes up the sun's own corona.
* [http://dwightronan.multiply.com/photos/album/23/ring-like_cloud_formation_around_the_full_moon Halo in the Philippines (November 23, 2007)]
* [http://valeriu.tihai.md/?p=280 Halo in Chisinau Moldova (photo and video]
* [http://www.atoptics.co.uk/halosim.htm Halo explanations and image galleries] at [http://www.atoptics.co.uk/ Atmospheric Optics]
* [http://haloreports.blogspot.com Halo reports of interesting halo observations around the World]
* [http://antwrp.gsfc.nasa.gov/apod/ap011107.html Astronomy Picture of the Day, November 7, 2001]
* [http://www.islandnet.com/~see/weather/eyes/pillars.htm Light Pillars]
* [http://www.astronomy.net.nz Southern Hemisphere Halo and other atmospheric phenomena]
* [http://www.enchantedceiling.com/PX5HCHUE86 Halo photo on EnchanteCeiling.com]
* [http://www.meteoros.de/haloe.htm Catalog with Photos of Types of Halos]
* [http://www.philiplaven.com/p2c1a.html How are glories formed?]
* [http://www.lumis.com/tag/Moon_Ring/page1/ Moon Halo Gallery]
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