A subsun (also spelled sub-sun) is an optical phenomenon that appears as a glowing spot visible within clouds or mist when observed from above. The subsun appears directly below the actual Sun, and is caused by sunlight reflecting off numerous tiny ice crystals suspended in the atmosphere. As such, the effect belongs to the family of halos.
Formation
The subsun phenomena appears when a region of hexagonal ice crystals act as a large mirror, creating a virtual image of the Sun below the horizon. As they fall through the air, the ice forms plate crystals which orient horizontally, i.e., with their hexagonal surfaces parallel to the Earth's surface. When they are disturbed by turbulence, the plates "wobble", causing their surfaces to deviate some degrees from the ideal horizontal orientation, and causing the reflection (i.e., the subsun) to become elongated vertically.
Deformations
When the subsun is stretched far enough vertically, it can become a vertical column known as a lower sun pillar. A sun pillar is a form of light pillar.
Examples (Images)
-
A vertically stretched subsun, seen from an airplane
-
A rounder subsun, partially obstructed by a gradual mountain peak
-
A more vertically elongated subsun before a gentle, snow-covered cliff
-
Seen to the bottom right is a plump, oval-shaped subsun, tiny in composition.
.JPG)
See also
References
- ^ Naylor (2002). Out of the Blue. Press Syndicate of the University of Cambridge. pp. 140, 152–154.
- ^ Greenler (1989). Rainbows, Halos, and Glories. Press Syndicate o/ UoC. pp. 65–68, 73–74.
- ^ Tape (1990). Atmospheric Halos. American Geophysical Union. p. 69.
 | This optics-related article is a stub. You can help Misplaced Pages by expanding it. |