Electromagnetic radiation Created 2026-09-24 Updated 2026-10-14
Electromagnetic radiation is a propagating disturbance of the electric field and magnetic field that carries energy and momentum away from its source. It can be a sustained electromagnetic wave or a finite wave packet: periodic oscillation is not required. In vacuum the disturbance travels at the speed of light. A receiver responds to fields arriving now from an earlier source event, as expressed by retarded time. This is how electrical activity at one place can deliver energy and information elsewhere without a connecting wire.
Stored electromagnetic energy alone does not establish outgoing electromagnetic radiation. A stationary electric charge in electrostatics, or a steady localized electric current in magnetostatics, can store electromagnetic energy with zero Poynting vector. Static combinations can have circulating energy flux without net outward power. Near a changing source, reactive energy can return later. The near and far field distinction separates these contributions from outgoing radiation zone fields.[ref]
Chapter 27: Field Energy and Field Momentum. §27-5, Fig. 27-6: static fields with circulating energy flux
A single traveling vacuum plane electromagnetic wave obeying the Maxwell equations has . Its Poynting vector gives the energy density and flux of a plane electromagnetic wave:Here is wave intensity; and are vacuum permittivity and vacuum permeability. For a monochromatic wave with linear polarization and peak amplitude , squared cosine averages to . Pulses require the instantaneous Poynting vector; arbitrary incident-and-reflected superpositions need not obey this relation.[ref]
Chapter 27: Field Energy and Field Momentum. §27-5, Eqs. (27.16)–(27.18): traveling-wave energy flux
The electromagnetic momentum density is . Completely absorbing a unidirectional vacuum pulse of energy transfers momentum ; see radiation pressure on a perfectly absorbing surface. A calculated pulse transfers . Symmetric emission can lose energy without net recoil because opposite momenta cancel.[ref]
The direction of emission matters as much as its total power. For an oscillating electric dipole moment along , the angular distribution of electric dipole radiation is strongest across the axis and vanishes along it. Its origin is geometric: the electric dipole radiation field is the transverse projection of the second time derivative of the electric dipole moment, so its magnitude contains . Squaring this electric field to obtain wave intensity gives . The electric-dipole approximation for radiation requires a source much smaller than its wavelength and observation in the radiation zone. [ref]
Chapter 28: Electromagnetic Radiation. Feynman, Leighton and Sands, Electromagnetic Radiation, §§28-2–28-3: transverse acceleration and dipole geometry
Normalized angular pattern of electric dipole radiation
. Calculated radiation zone model, not measured data. The polar curve's radial coordinate is normalized power per solid angle, , rather than physical distance or a field line. The angle is measured from the dipole axis. Rotating this meridional pattern about that axis gives the three-dimensional angular distribution. Details.For example, the power per solid angle at is one quarter of its equatorial value, while the electric field amplitude is one half. To normalize the angular distribution to total power, use spherical coordinates with :The integral follows by substituting , giving . This is a probability-like normalization over direction, with units of inverse steradian; it does not make the dipole an isotropic radiator. The same angular integral underlies the Larmor formula for nonrelativistic accelerated electric charge.
Detection requires the incident electromagnetic field to do something observable. An antenna develops an electrical response; a thermopile converts absorbed energy into a thermal and then electrical signal; a photodetector can respond through photon absorption. Hertz spark transmission and detection experiment makes this conversion visible as a tiny spark. Detector orientation, sensitivity, and surrounding reflections all matter: failure to see a signal does not prove that no electromagnetic radiation reached the receiver.
Past exam of the mathematics course of the University of Cambridge 2020 ii Paper 3 36D ii Solution Created 2026-09-24 Updated 2026-09-29
In the radiation zone, both fields are transverse to and obeyThe outward Poynting vector isso its time average isAn absorbing shell receives the incident momentum rather than reversing it. Hence radiation pressure on a perfectly absorbing surface givesAt ,and thereforeIf is the angle between and , this isIts spherical average is ; the vector force integrates to zero by the inversion symmetry of the electric dipole radiation pattern.
For a sinusoidal plane electromagnetic wave in vacuum, write the maximum electric field as . The magnetic field maximum is , so the cycle-averaged Poynting vector magnitude, or light intensity, isEach photon carries energy , where is the Planck constant. Therefore the photon number flux density, namely the number per unit normal area per unit time, isMultiplying by an illuminated normal area gives the photon arrival rate. Each absorbed photon transfers momentum at normal incidence, giving the radiation pressure on a perfectly absorbing surfaceThese are time-averaged quantities. At oblique angle of incidence , the normal radiation pressure is ; the simple displayed expression assumes normal incidence.
Radiation pressure Created 2026-09-28 Updated 2026-10-14
Radiation pressure is the normal momentum flux transferred by electromagnetic radiation to a surface. A photon travelling in vacuum carries momentum , where is its energy, its frequency, the Planck constant and the speed of light. Photon absorption transfers that momentum; specular reflection reverses its normal component. This lets light exert a force even when almost no energy becomes heat in the receiver.
Two useful formulas describe different preparations. A directed beam normally incident on a stationary perfect absorber gives pressure , and on a stationary perfect mirror gives . Here is light intensity, the incident power per beam cross-sectional area perpendicular to propagation, in . An isotropic photon gas has pressure , where is its radiation internal energy per volume, in . Stored energy density and travelling energy flux must be distinguished: an isotropic field can have zero net energy flux and positive radiation pressure.
The physical appeal is that the same momentum conservation connects a single photon collision, a mirror's measurable force, and a radiation-filled cavity's equation of state. The directional calculation below complements radiation pressure on a perfectly absorbing surface; the equilibrium spectrum and its temperature dependence belong to blackbody radiation and the photon gas.
