White sunlight bends, splits into colors and reflects inside a raindrop. Follow in 14 scenes why that light bunches up at about 42°, why a rainbow is an arch, and where a double rainbow comes from.
Watch from the start in 3DA rainbow needs two things: sunlight, and countless raindrops hanging in the sky.
A rainbow needs sunlight and raindrops
View in 3D →White sunlight holds many colors
View in 3D →Zooming in on one drop among many
View in 3D →Light bends as it enters the drop, reflects off the back, and bends again on the way out.
Light slows down in water and changes direction
View in 3D →Violet bends a little more than red
View in 3D →Most light leaks out; only a little reflects
View in 3D →Each color leaves the drop in its own direction
View in 3D →Light leaving a raindrop bunches up at one angle. That angle decides where the rainbow appears.
A different entry height means a different exit angle
View in 3D →Light piles up near the largest angle
View in 3D →The sky shines 42° from your head’s shadow
View in 3D →Red comes from higher drops, violet from lower ones
View in 3D →Join every direction at that angle and you get a cone. With no ground in the way, a rainbow is a full circle.
The ground cuts the 42° cone into an arch
View in 3D →With no ground in the way, a full circle
View in 3D →An outer rainbow made by light that reflects twice
View in 3D →More in the series
The numbers come from the refractive index formula for water (IAPWS 1997) and the laws of refraction (Snell) and reflection (Fresnel). In the 3D view, the raindrop and the spreading of colors inside it are drawn larger so you can see them.