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Why are skies blue?

Published in Atmospheric Optics 2 mins read

The sky is blue because of a phenomenon called Rayleigh scattering, where shorter wavelengths of visible light are scattered more efficiently than longer wavelengths.

Understanding Rayleigh Scattering

Sunlight, which appears white, is actually composed of all the colors of the rainbow. As this sunlight enters the Earth's atmosphere, it collides with air molecules (primarily nitrogen and oxygen). This collision causes the light to scatter in different directions.

Why Blue Specifically?

  • Shorter Wavelengths: Blue and violet light have shorter wavelengths compared to other colors like red and orange.
  • More Scattering: As stated in the reference, "Blue light is scattered more than the other colors because it travels as shorter, smaller waves." This means blue light is scattered much more effectively than other colors when it hits air molecules.
  • Violet Absorption: While violet light is scattered even more than blue light, our eyes are less sensitive to violet, and some violet light is absorbed by the upper atmosphere.

Summary Table: Light Scattering

Color Wavelength Scattering Effect Visibility
Violet Shortest Most Low
Blue Short High High
Green Medium Moderate Moderate
Yellow Long Low Low
Orange Longer Less Less
Red Longest Least Least

Other Factors Affecting Sky Color

While Rayleigh scattering primarily explains the blue sky, other factors can influence the sky's appearance.

  • Sunrise and Sunset: At sunrise and sunset, the sunlight travels through a greater distance in the atmosphere. Most of the blue light is scattered away, leaving the longer wavelengths like orange and red to dominate, creating the beautiful sunrise and sunset colors.
  • Pollution: Particles in polluted air can also scatter light, sometimes making the sky appear hazy or white.
  • Cloud Cover: Clouds block and scatter sunlight, which can make the sky appear grey or white.

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