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== Dipole radiation == [[File:Electric dipole radiation.gif|thumb|Modulus of the Poynting vector for an oscillating electric dipole (exact solution). The two charges are shown as two small black dots.]] <!-- use of the far-field approximation for the near field yielded incorrect results, see archived discussion [[File:dipole.gif|thumb|right|250px|Evolution of the magnetic field of an oscillating electric dipole. The field lines, which are horizontal rings around the axis of the vertically oriented dipole, are perpendicularly crossing the ''xy''-plane of the image. Shown as a colored [[Contour line|contour plot]] is the ''z''-component of the field. Cyan is zero magnitude, green–yellow–red and blue–pink–red are increasing strengths in opposing directions.]] --> {{see also|Dipole antenna}} In addition to dipoles in electrostatics, it is also common to consider an electric or magnetic dipole that is oscillating in time. It is an extension, or a more physical next-step, to [[spherical wave]] radiation. In particular, consider a harmonically oscillating electric dipole, with [[angular frequency]] ''ω'' and a dipole moment ''p''<sub>0</sub> along the '''ẑ''' direction of the form : <math>\mathbf{p}(\mathbf{r}, t) = \mathbf{p}(\mathbf{r})e^{-i\omega t} = p_0\hat{\mathbf{z}}e^{-i\omega t} .</math> In vacuum, the exact field produced by this oscillating dipole can be derived using the [[retarded potential]] formulation as: : <math>\begin{align} \mathbf{E} &= \frac{1}{4\pi\varepsilon_0} \left\{ \frac{\omega^2}{c^2 r} \left( \hat{\mathbf{r}} \times \mathbf{p} \right) \times \hat{\mathbf{r}} + \left( \frac{1}{r^3} - \frac{i\omega}{cr^2} \right) \left( 3\hat{\mathbf{r}} \left[\hat{\mathbf{r}} \cdot \mathbf{p}\right] - \mathbf{p} \right) \right\} e^\frac{i\omega r}{c} e^{-i\omega t} \\ \mathbf{B} &= \frac{\omega^2}{4\pi\varepsilon_0 c^3} (\hat{\mathbf{r}} \times \mathbf{p}) \left( 1 - \frac{c}{i\omega r} \right) \frac{e^{i\omega r/c}}{r} e^{-i\omega t}. \end{align}</math> For {{sfrac|''rω''|''c''}} ≫ 1, the far-field takes the simpler form of a radiating "spherical" wave, but with angular dependence embedded in the cross-product:<ref>[[David J. Griffiths]], Introduction to Electrodynamics, Prentice Hall, 1999, page 447</ref> : <math>\begin{align} \mathbf{B} &= \frac{\omega^2}{4\pi\varepsilon_0 c^3} (\hat{\mathbf{r}} \times \mathbf{p}) \frac{e^{i\omega (r/c - t)}}{r} = \frac{\omega^2 \mu_0 p_0 }{4\pi c} (\hat{\mathbf{r}} \times \hat{\mathbf{z}}) \frac{e^{i\omega (r/c - t)}}{r} = -\frac{\omega^2 \mu_0 p_0 }{4\pi c} \sin(\theta) \frac{e^{i\omega (r/c - t)}}{r} \mathbf{\hat{\phi}} \\ \mathbf{E} &= c \mathbf{B} \times \hat{\mathbf{r}} = -\frac{\omega^2 \mu_0 p_0}{4\pi} \sin(\theta) \left(\hat{\phi} \times \mathbf{\hat{r}}\right) \frac{e^{i\omega (r/c - t)}}{r} = -\frac{\omega^2 \mu_0 p_0}{4\pi} \sin(\theta) \frac{e^{i\omega (r/c - t)}}{r} \hat{\theta}. \end{align}</math> The time-averaged [[Poynting vector]] : <math>\langle \mathbf{S} \rangle = \left(\frac{\mu_0 p_0^2\omega^4}{32\pi^2 c}\right) \frac{\sin^2(\theta)}{r^2} \mathbf{\hat{r}}</math> is not distributed isotropically, but concentrated around the directions lying perpendicular to the dipole moment, as a result of the non-spherical electric and magnetic waves. In fact, the [[spherical harmonic]] function (sin ''θ'') responsible for such [[torus|toroidal]] angular distribution is precisely the ''l'' = 1 "p" wave. The total time-average power radiated by the field can then be derived from the Poynting vector as : <math>P = \frac{\mu_0 \omega^4 p_0^2}{12\pi c}.</math> Notice that the dependence of the power on the fourth power of the frequency of the radiation is in accordance with the [[Rayleigh scattering]], and the underlying effects why the sky consists of mainly blue colour. A circular polarized dipole is described as a superposition of two linear dipoles.
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