SUMMARY
The circular shape of rainbows is a result of light refraction and reflection within water droplets, specifically at angles of 40-42 degrees relative to the observer's line of sight. While rainbows appear as semicircles due to the horizon obstructing the lower half, they can be seen as full circles from high altitudes, such as in an airplane, where the phenomenon is referred to as a "glory." Unlike rainbows, glories are caused by back-scattering of light and exhibit different angular sizes and color orders. The physics behind rainbows is well-understood, while the nature of glories remains a topic of ongoing debate.
PREREQUISITES
- Understanding of light refraction and reflection principles
- Familiarity with the concepts of angles, specifically 40-42 degrees
- Knowledge of atmospheric optical phenomena, including rainbows and glories
- Basic comprehension of spherical symmetry in raindrops
NEXT STEPS
- Research the physics of light refraction in water droplets
- Explore the differences between rainbows and glories in detail
- Study atmospheric optics and related phenomena
- Investigate the role of ice crystals in creating non-circular optical effects
USEFUL FOR
Students of physics, meteorologists, and anyone interested in atmospheric phenomena and optical science will benefit from this discussion.