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Rayleigh scattering

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Rayleigh scattering

Dispersion of electromagnetic radiation by particles with radii less than ¹⁄₁₀ the wavelength of the radiation. It is named for Baron Rayleigh, who described it in 1871. Since blue light is at the short wavelength end of the visible spectrum, it is scattered in the atmosphere much more than the longer-wavelength red light. This causes the blue colour of the sky, since the observer sees only the scattered light. The Rayleigh laws predict the variation of the intensity and the polarization of scattered light.


Rayleigh scattering [′rā·lē ‚skad·ə·riŋ]
(electromagnetism)
Scattering of electromagnetic radiation by independent particles which are much smaller than the wavelength of the radiation.


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Our planet looks blue because of Rayleigh scattering of sunlight by the atmosphere.
As the pulse travels along the fiber, some of the light is lost via absorption and Rayleigh scattering.
The sensors operate on the optical time domain reflectometry (OTDR) principle, invented by Barnowski and Jensen in 1976, which was the first method for distributed fibre measurements using backward Rayleigh scattering to determine the optical loss along fibres [19].
 
 
 
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