Why the Sky Changes Colour

Written by Studio AM.

On a clear day, the sky overhead looks blue. Near sunset, the light around the sun can look orange or red. Both colours are linked to scattering: air molecules redirect some of the sunlight passing through the atmosphere.

Sunlight contains different wavelengths. Nitrogen and oxygen molecules are much smaller than these light waves, and they scatter shorter wavelengths more strongly than longer ones. The process is biased toward the shorter wavelengths. Blue light is therefore scattered more strongly than red light. Some of that scattered blue light reaches our eyes from across the sky.

At sunset, sunlight travels through a longer path in the atmosphere. More blue light is scattered out of the direct beam before it reaches us. Longer wavelengths make up a greater share of the remaining light, so orange and red become more noticeable near the sun. These colours were already in the sunlight; the longer path changes their relative share of the visible spectrum.

Clouds and particles can also affect the colours. Scattering by air molecules explains the basic clear-sky pattern, not every detail of every sunset.

Questions

Choose an answer. The explanation appears after you answer.

  1. Question 1 of 4

    What does the passage set out to explain?

  2. Question 2 of 4

    Why can light near sunset look less blue?

  3. Question 3 of 4

    If far fewer air molecules scattered sunlight, how would a clear daytime sky look?

  4. Question 4 of 4

    The passage calls scattering 'biased'. Here that means the process:

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