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and remembering that r   r for r in the far zone, we can use the leading terms of a
                        binomial expansion of the square root to get

                                                      
    2
                                              2(ˆ r · r )  r         2(ˆ r · r )    ˆ r · r


                                   R = r 1 −        +       ≈ r 1 −         ≈ r 1 −
                                                r       r              r             r

                                     ≈ r − ˆ r · r .                                           (6.19)
                        Thus the Green’s function may be approximated as
                                                               e − jkr
                                                                     jkˆ r·r
                                                    G(r|r ; ω) ≈   e    .                      (6.20)
                                                               4πr
                        Here we have kept the approximation (6.19) intact in the phase of G but have used
                        1/R ≈ 1/r in the amplitude of G. We must keep a more accurate approximation for

                        the phase since k(ˆ r · r ) may be an appreciable fraction of a radian. We thus have the
                        far-zone approximation for the vector potential
                                                          e − jkr        jkˆ r·r
                                            ˜
                                                                 ˜ i


                                            A e (r,ω) ≈ ˜µ(ω)    J (r ,ω)e   dV ,
                                                          4πr   V
                        which we may use in computing (6.18).
                          Let us summarize the expressions for computing the far-zone fields:

                                             ˜
                                                                       ˆ ˜
                                                           ˆ ˜
                                             E(r,ω) =− jω θA eθ (r,ω) + φA eφ (r,ω) ,          (6.21)
                                                          ˜
                                                      ˆ r × E(r,ω)
                                             ˜
                                             H(r,ω) =           ,                              (6.22)
                                                          η
                                                      e − jkr
                                             ˜
                                            A e (r,ω) =    ˜ µ(ω)˜ a e (θ,φ,ω),                (6.23)
                                                       4πr

                                                         ˜ i


                                          ˜ a e (θ, φ, ω) =  J (r ,ω)e jkˆ r·r    dV .         (6.24)
                                                       V
                        Here ˜ a e is called the directional weighting function. This function is independent of r
                        and describes the angular variation, or pattern, of the fields.
                                       ˜ ˜
                          In the far zone E, H, ˆ r are mutually orthogonal. Because of this, and because the fields
                        vary as e − jkr /r, the electromagnetic field in the far zone takes the form of a spherical
                        TEM wave, which is consistent with the Sommerfeld radiation condition.
                        Power radiated by time-harmonic sources in unbounded space. In § 5.2.1 we
                        defined the power radiated by a time-harmonic source in unbounded space as the total
                        time-average power passing through a sphere of very large radius. We found that for a
                        Hertzian dipole the radiated power could be computed from the far-zone fields through
                                                         2π  π

                                                                    2
                                              P av = lim      S av · ˆ rr sin θ dθ dφ
                                                   r→∞
                                                        0   0
                        where
                                                           1
                                                                ˇ
                                                                    ˇ ∗
                                                     S av =  Re E × H
                                                           2
                        is the time-average Poynting vector. By superposition this holds for any localized source.
                        Assuming a lossless medium and using phasor notation to describe the time-harmonic

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