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Heat & Temperature · Concept

Thermal Radiation

Reading time: 9 minConfidence: HighLast verified: October 2026

Thermal radiation is electromagnetic radiation emitted by matter as a consequence of its temperature, produced by the thermal motion of charged particles. An ideal emitter, a black body, has a spectrum given by Planck's law and determined by temperature alone; its total emitted power per unit area is σT4 (Stefan–Boltzmann law) and its spectral peak lies at wavelength λmax = b/T (Wien's displacement law). Real surfaces emit a fraction ε (the emissivity) of the black-body value.

Curious

One sentence that captures itEverything glows with light set by its temperature: you glow in the infrared, a stove ring glows red, and the Sun glows white-yellow.

All objects constantly emit electromagnetic radiation, because the charged particles inside them jiggle with heat. At room temperature that radiation is invisible infrared, which is what thermal cameras detect. Heat something to about 800 K and it starts to glow dull red; hotter still, it glows orange, then yellow-white. The colour of a hot object tells you its temperature, which is how astronomers measure the surface temperatures of stars (see Hertzsprung-Russell Diagram).

Thermal radiation needs no medium, which is how the Sun warms Earth across empty space (see Heat Transfer). Explaining its spectrum required the birth of quantum theory in 1900 (see Max Planck).

Exploring

Worked examples(1) Peak wavelengths from Wien's law, λmax = 2.898×10−3 m K / T: the Sun (5,772 K) peaks near 502 nm (green-blue light); a person (310 K) near 9.3 μm (infrared); the cosmic microwave background (2.7255 K) near 1.06 mm (microwaves). (2) Stefan–Boltzmann check: L = 4πR²σT4 with R = 6.957×108 m and T = 5,772 K gives 3.83×1026 W, the IAU nominal solar luminosity. (3) Earth: absorbing 1,361 W/m² sunlight with albedo 0.30 and radiating as a black body gives T = [S(1−A)/4σ]1/4 ≈ 255 K, about 33 K colder than the observed mean surface temperature of about 288 K; the difference is the natural greenhouse effect. (Computed in Python.)
LawStatementYear
Kirchhoff's lawEmissivity equals absorptivity at each wavelength (equilibrium)1859
Stefan–Boltzmann lawEmitted power per area = εσT41879 / 1884
Wien's displacement lawλmaxT = 2.898×10−3 m K1893
Planck's lawFull spectrum of black-body radiation1900
Common mistake — Commonly ConfusedA black body is not necessarily black to the eye: the Sun is a good approximation to a black body. “Black” refers to perfect absorption, which by Kirchhoff's law implies perfect emission. Also, the peak of the spectrum depends on whether it is plotted per unit wavelength or per unit frequency, so “the Sun peaks in green” is true only in the wavelength convention.

Deep Dive

Primary sourcePlanck, M. (1901). “Über das Gesetz der Energieverteilung im Normalspectrum.” Annalen der Physik, 309, 553–563.

Planck's law. The spectral radiance is Bλ(T) = (2hc²/λ5)/(ehc/λkBT − 1). Classical equipartition (the Rayleigh–Jeans law) instead predicted radiance growing without limit at short wavelengths, the “ultraviolet catastrophe” (see Equipartition Theorem). Planck's assumption that oscillator energies come in units of hf removed the divergence; integrating his law gives the Stefan–Boltzmann constant σ = 2π5kB4/(15c²h³) = 5.670×10−8 W m−2 K−4, and differentiating it gives Wien's law.

Cosmic test. The COBE FIRAS instrument (1990) measured the cosmic microwave background spectrum as a black body at 2.725 K with deviations below about 50 parts per million, the most precise black-body spectrum ever recorded (see Cosmic Microwave Background). Stars are only approximate black bodies; their spectra show absorption lines and their “effective temperature” is defined through the Stefan–Boltzmann law (see Red Giants).

Greenhouse effect. Earth's surface emits mostly between about 5 and 50 μm, where water vapour and carbon dioxide absorb strongly; these gases re-emit infrared both upward and downward, raising the surface temperature above the 255 K radiative estimate. The physics of this effect is well established; projections of future warming depend on feedbacks, especially clouds, that carry larger uncertainties, as assessed by the IPCC.

Sources

  • Planck, M. (1901). Annalen der Physik, 309, 553–563.
  • Mather, J.C., et al. (1994). “Measurement of the Cosmic Microwave Background Spectrum by the COBE FIRAS Instrument.” The Astrophysical Journal, 420, 439–444.
  • Prša, A., et al. (2016). “Nominal values for selected solar and planetary quantities: IAU 2015 Resolution B3.” The Astronomical Journal, 152, 41.
Last verified: October 2026 · Source: Planck (1901); Mather et al. (1994); IAU 2015 B3 · Confidence: high