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 to the incident direction. It is less partially polarized at other scattering angles.