Science · Level 4 · 209 words
The Colour Of Air
Original passage © Studio AM, written for Fluency.
Air has no colour of its own, yet the sky overhead is blue and the same sky turns orange at the end of the day. Both facts come from one process, and that process depends on size.
Sunlight is a mixture of wavelengths, and the molecules of nitrogen and oxygen in the air are far smaller than any of them. When a wave meets a particle much smaller than itself, the particle does not block the wave; it takes in a little energy and sends it out again in every direction. This redirection is called scattering, and it is biased: the shorter the wavelength, the more it is scattered. Blue light, being short, is thrown sideways across the whole sky, while red light mostly continues straight ahead. Looking anywhere except at the sun, you see the light that was scattered, so you see blue.
At sunset the geometry changes. The sun sits low, so its light crosses far more air before it reaches you, and the blue is scattered away long before it arrives. What survives the journey is the long end of the spectrum. The orange of a sunset is not something added to the light; it is what is left after the blue has been taken out.
Source: Written for Fluency. Original passage © Studio AM, written for Fluency.