The incident light can be decomposed into two orthogonal linear
polarizations respectively parallel and perpendicular to the plane of
the page as shown in Figure 16.6.
An observer O located at to the incident direction
observes the scattered light. The dipole produced by the parallel
component of the incident
does not produce any
at
the observer O. The observer O receives radiation only from the dipole
oscillations perpendicular to the plane of the paper. The scattered
radiation received at O is linearly polarized perpendicular to the
plane of the paper.
During daytime the sky appears illuminated because of the sunlight scattered by the atmosphere (Figure 16.7).
The scattered light is polarized by the mechanism discussed here. The polarization is maximum (although not completely plane polarized) when the light is scattered at