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Scattering of Light in Atmosphere
When a beam of light falls in an atom, it causes the electrons in the atom to vibrate. The vibrating electrons, in turn, re-emit light in all direction.
As shown in fig (a). This process is called Scattering. Earth’s atmosphere contains air molecules and other tiny particles. When light from the sun passes through the atmosphere, it gets scattered by the large number of particles in the intensity of scatters light varies inversely as the fourth power of the wavelength of light.
Scattered Radiation
Fig (a)
(I) Blue color of sky : Since the wavelength of *blue color is smaller then the wavelength of red color (λv < λr ) , Scattering of blue light by particles in earth's atmosphere is very large. For this reason we see a blue sky
(II) Clouds are white: A cloud is composed of large dust practices and water molecules these large size d particles do not obey Raleigh law of Scattering. Therefore, all colors or wavelength are scattered equally. The overall result is a white cloud.
Scattered Radiation2
Fig (b)
(III) Sun looks reddish at sunset or sunrise: At the time of sunset or sunrise ,the sun near horizon as shown in fig (b), the rays from the sun must travel more blue is scattered from the sunlight. The removal of blue leaves the transmitted light more reddish in appearance. Therefore, sun looks reddish at the sunset or sunrise.
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