Have you ever looked up after a rainstorm and seen a beautiful arc of colors across the sky? That’s a rainbow — a natural light show created by the interaction of sunlight and water droplets. But what exactly causes this colorful phenomenon? The answer lies in physics.
To see a rainbow, three basic conditions must be met:
When these conditions are just right, light interacts with the droplets to produce the rainbow.
The formation of a rainbow involves three main physical processes:
When sunlight enters a water droplet, it bends because light changes speed when moving from air to water. This bending is called refraction.
As light refracts, it splits into its component colors because each color bends by a slightly different amount. This separation of white light into colors is known as dispersion.
Inside the droplet, light reflects off the back surface of the droplet and travels back toward the front.
As the reflected light exits the droplet, it refracts again, further separating the colors.
The angle at which the light exits the droplet determines the color we see:
The result is a circular arc of colors with Red on the outside and Violet on the inside:
ROYGBIV – Red, Orange, Yellow, Green, Blue, Indigo, Violet
Yes and no! A rainbow is actually a full circle of light, but we usually only see the upper arc because the ground blocks the bottom half. If you’re in a plane or on a mountain, you might see a full circular rainbow.
Written by Vidhathri