Blue Sky
Air molecules scatter short-wavelength (blue/violet) light in all directions. You see scattered blue everywhere except toward the sun.
Module 04
Air molecules scatter shorter wavelengths far more than longer ones. That single fact explains a surprising amount of what you see in the sky.
At noon (high sun), light takes the shortest path — the sky looks light blue/white. Near sunset, the path is long: most blue is scattered away, leaving the red end to reach you.
Scattered intensity ≈ 2.23× green.
Air molecules scatter short-wavelength (blue/violet) light in all directions. You see scattered blue everywhere except toward the sun.
At the horizon, sunlight travels a long path. Blue is scattered out; only red reaches you directly.
Shortest atmospheric path — little selective scattering — direct light looks nearly white.
Water droplets are larger than the wavelength of light — they scatter all colours equally.
No atmosphere means no scattering. Away from the sun, the sky is black.
Earth looks blue (scattered sunlight from its atmosphere) against the black sky of space.
Red light has the longest visible wavelength, so it is scattered the least — it travels farther through fog, smoke and dust.