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Rayleigh scattering
Rayleigh scattering is the scattering of light or other electromagnetic radiation by particles much smaller than the wavelength of the radiation. It is named after Lord Rayleigh, who first proposed a mathematical theory of this effect in 1871. Rayleigh scattering usually occurs when the radiation is scattered by particles with a size much smaller than the wavelength of the radiation, such as molecules of air or particles in a suspension. This type of scattering results in a decrease in intensity and color shift in the scattered light, which is why the sky appears blue and sunsets appear red.
Rayleigh scattering is the scattering of light or other electromagnetic radiation by particles much smaller than the wavelength of the radiation. It is named after Lord Rayleigh, who first proposed a mathematical theory of this effect in 1871. Rayleigh scattering usually occurs when the radiation is scattered by particles with a size much smaller than the wavelength of the radiation, such as molecules of air or particles in a suspension. This type of scattering results in a decrease in intensity and color shift in the scattered light, which is why the sky appears blue and sunsets appear red.
Rayleigh scattering is the scattering of light or other electromagnetic radiation by particles much smaller than the wavelength of the radiation. It is named after Lord Rayleigh, who first proposed a mathematical theory of this effect in 1871. Rayleigh scattering usually occurs when the radiation is scattered by particles with a size much smaller than the wavelength of the radiation, such as molecules of air or particles in a suspension. This type of scattering results in a decrease in intensity and color shift in the scattered light, which is why the sky appears blue and sunsets appear red.
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