SCATEERING OF LIGHT
Atoms or molecules which are
exposed to light absorb light energy and emit some part of the light energy in
different directions. This is the basic process happens in scattering of light.
The effect of
light on a molecule or an atom depends on the size of atom or molecule. If the
size of the particle (atom or molecule) is small, it will be affected by higher
frequency (lower wave length) light and vice versa.
Actually we can
see different colours because of scattering of light. When molecular size (of
the molecules of an object) are comparable to wave length of a particular
colour then that object will scatter that particular colour.
Let us observe some examples in the nature.
BLUE COLOUR OF SKY
We know that our atmosphere contains
different types of molecules and atoms. The reason for blue sky is due to the
molecules N2 and O2. The sizes of these molecules are
comparable to the wavelength of blue light. These molecules act as scattering
centres for scattering of blue light.
WHY SKY APPEARS WHITE SOMETIMES?
Our atmosphere contains
atoms and molecules of different sizes. According to their sizes, they are able
to scatter different wavelengths of light. For example, the size of the water
molecule is greater than the size of the N2 or O2. It
acts as a scattering centre for other frequencies which are lower than the
frequency of blue light.
On a hot day, due
to rise in the temperature water vapour enters into atmosphere which leads to
abundant presence of water molecules in the atmosphere. These water molecules
scatter the colours of other frequencies (other than blue). All such colours of
other frequencies reach your eye and the sky appears white. (As blue is already
scattered by N2 and O2 molecules these remaining colours
scattered by water vapour combine with blue to form white colour).
WHY SUN APPEARS RED DURING SUNSET AND SUN RAISE
The atmosphere
contains free molecules and atoms with different sizes. These molecules and
atoms scatter light of different wavelengths which are comparable to their
size. Molecules having a size that is comparable to the wavelength of red light
are less in the atmosphere. Hence scattering of red light is less when compared
to the other colours of light. The light from the sun needs to travel more
distance in atmosphere during sunrise and sunset to reach your eye. In morning
and evening times, during sunrise and sunset, except red light all colours
scatter more and vanish before they reach you. Since scattering of red light is
very small, it reaches you. As a result sun appears red in colour during
sunrise and sunset.
WHY SUN DOESN’T APPEAR RED IN COLOUR DURING NOON
During noon hours, the distance to be
travelled by the sun rays in the atmosphere is less than that compared to
morning and evening hours. Therefore all colours reach your eye without much
scattering. Hence the sun appears white during noon hours.
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