The Earth’s atmosphere contains tiny
molecules of gas and dust particles. Sunlight
entering the atmosphere hits these molecules
and dust particles. Colours with longer
wavelengths, like red and yellow, can pass
through the atmosphere without being
scattered by these molecules of gas and dust
particles. But the colour blue, with its shorter
wavelength, is scattered by the gas molecules
and the dust in the upper atmosphere.
This is why the sky appears blue.
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