Corona (optical phenomenon)
From Wikipedia, the free encyclopedia
(Redirected from Corona (meteorology))
For other uses, see Corona (disambiguation).
In meteorology, a corona is produced by the diffraction of light from either the Sun or the Moon by individual small water droplets (and sometimes tiny ice crystals) of a cloud.
The corona consists of small number of concentric colored rings around the celestial object and a central bright aureole. The angular size of the corona depends on the diameters of the cloud droplets - small droplets produce bright coronae. Coronae differ from haloes in that the latter are formed by refraction (rather than diffraction) from comparatively large rather than small ice crystals. Reddish colors always occupy the outer part of a corona's ring. (This is an atmospheric Airy disc.)
[edit] See also
[edit] External links
- Explanation and image gallery - Atmospheric Optics by Les Cowley
- Rings around the sun and moon: coronae and diffraction
- Corona from Fogged Eyeglasses
- Experimental simulations of pollen coronas
- The Corona
[edit] Gallery
-
Solar Corona at Golden Gate Bridge
-
Partial Corona at Golden Gate Bridge
| This optics-related article is a stub. You can help Wikipedia by expanding it. |
| This climatology/meteorology-related article is a stub. You can help Wikipedia by expanding it. |