The daytime sky on Earth
appears blue in colour. Light is made up of PHOTONS which are matterless
particles. White light is made up of seven colours: red, orange, yellow, green, blue, violet & indigo.
This light travels at
different wavelengths. Some colours are better at passing through gases than
others. Red light is seen at longer wavelengths and indigo has the shortest
wavelength.
When photons from the Sun
travel into Earth's atmosphere some of this light hits and bounces the nitrogen
and oxygen molecules there. The result is that light is split up and scattered.
Red, orange, yellow and
green light carries straight on through this atmosphere but blue, violet and
indigo get bounced around from molecule to molecule.
We see a blue sky as a
result of all this bouncing around.
Why don't we see an Indigo
or Violet sky? Simply because our eyes do not see these colours very well. Blue
is a more dominant colour.
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