Rainbow — Core Principles
Core Principles
A rainbow is a natural optical phenomenon caused by the interaction of sunlight with atmospheric water droplets. It involves three key processes: dispersion, refraction, and total internal reflection.
White sunlight, a mixture of colors, first enters a raindrop and undergoes refraction, splitting into its constituent colors (dispersion) because each color bends at a slightly different angle. The light then travels to the back of the droplet, where it undergoes total internal reflection, bouncing back inside.
Finally, it exits the droplet, undergoing a second refraction, further separating the colors and directing them towards the observer. The primary rainbow, the brighter one, results from one internal reflection, showing red on the outside and violet on the inside, with an angular radius of about .
The secondary rainbow, fainter and larger, results from two internal reflections, with colors reversed (violet outside, red inside) and an angular radius of about . For a rainbow to be seen, the sun must be behind the observer, and water droplets must be in front.
Each observer sees a unique rainbow, as it's an optical effect, not a physical object.
Important Differences
vs Secondary Rainbow
| Aspect | This Topic | Secondary Rainbow |
|---|---|---|
| Number of Internal Reflections | One | Two |
| Relative Brightness | Brighter | Fainter |
| Order of Colors (Top to Bottom) | Red, Orange, Yellow, Green, Blue, Indigo, Violet (ROYGBIV) | Violet, Indigo, Blue, Green, Yellow, Orange, Red (VIBGYOR - inverted) |
| Angular Radius (approx. from anti-solar point) | $40^circ - 42^circ$ | $51^circ - 54^circ$ |
| Position Relative to Each Other | Inner arc | Outer arc |