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CHAPTER 11  The Uniform Plane Wave           397




















                          Figure 11.5 Plots of the electric field component magnitudes in Eq. (95) as
                          functions of z. Note that the y component lags behind the x component in z.
                          As time increases from zero, both waves travel to the right, as per Eq. (94).
                          Thus, to an observer at a fixed location, the y component leads in time.


                     magnitude at a distance of one wavelength in z (for fixed t)orata time t = 2π/ω
                     later (at a fixed z).
                         For illustration purposes, if we take the length of the field vector as a measure
                     of its magnitude, we find that at a fixed position, the tip of the vector traces out the
                     shape of an ellipse over time t = 2π/ω. The wave is said to be elliptically polarized.
                     Elliptical polarization is in fact the most general polarization state of a wave, since
                     it encompasses any magnitude and phase difference between E x and E y . Linear
                     polarization is a special case of elliptical polarization in which the phase difference
                     is zero.
                         Another special case of elliptical polarization occurs when E x0 = E y0 = E 0 and
                     when φ =±π/2. The wave in this case exhibits circular polarization.To see this,
                     we incorporate these restrictions into Eq. (94) to obtain
                                E(z, t) = E 0 [cos(ωt − βz)a x + cos(ωt − βz ± π/2)a y ]
                                      = E 0 [cos(ωt − βz)a x ∓ sin(ωt − βz)a y ]     (96)
                     If we consider a fixed position along z (such as z = 0) and allow time to vary, (96),
                     with φ =+π/2, becomes

                                        E(0, t) = E 0 [cos(ωt)a x − sin(ωt)a y ]     (97)

                     If we choose −π/2in (96), we obtain

                                        E(0, t) = E 0 [cos(ωt)a x + sin(ωt)a y ]     (98)

                     The field vector of Eq. (98) rotates in the counterclockwise direction in the xy plane,
                     while maintaining constant amplitude E 0 , and so the tip of the vector traces out a
                     circle. Figure 11.6 shows this behavior.
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