Access this content offline
Omniguides
Skip to the reading

Blackbody Radiation

Separate a thermal spectrum’s peak from its complete area and total emitted power.

AP Physics 2 Topic 15.4 · College Board CED printed p. 142, 143 / PDF p. 149, 150 · See this topic in the course outline

A warm object radiates a broad spectrum. The most prominent wavelength and total emitted power answer different questions.

Before you start

Thermal energy becomes a continuous radiation spectrum

Matter spontaneously transfers some internal thermal energy into electromagnetic radiation. A blackbody is an ideal absorber of all incident radiation. At thermal equilibrium it also emits radiation while its temperature remains constant because energy entering and leaving balance. “Black” refers to ideal absorption, not an insistence that a hot body must look dark.

A blackbody's continuous emission spectrum depends only on its temperature, not on a collection of isolated atomic transition lines. Real bodies approximate the ideal to varying degrees; their surface emissivity can make the emitted distribution differ. A filament's broad thermal spectrum and a dilute gas's separated line spectrum should not be modeled as the same thing.

Read the axis before comparing curves

Plot spectral intensity per unit wavelength on the vertical axis and wavelength on the horizontal axis. The curve's peak gives the wavelength with greatest emitted power per area per wavelength interval; it is not the only emitted wavelength. Adding the contributions from all wavelength intervals—graphically, the area under the entire curve—gives total emitted intensity. Multiplying that total by emitting surface area gives total power.

Classical continuous-energy predictions fail to reproduce the measured distribution, especially at short wavelengths. Planck's law uses quantized energy exchanges and gives a finite thermal spectrum. We use its qualitative shape without deriving it: as temperature rises, the curve increases and the peak shifts toward shorter λ. At a fixed T, doubling the surface area doubles total power but does not move the spectral peak or change the intensity per unit emitting area.

Blackbody comparisons using Wien and Stefan–Boltzmann laws
Temperature (K)Peak λ (μm)Total emitted intensity relative to 3000 K
30000.9661
45000.6445.0625
60000.48316

A sketch using these values places the hotter peak farther left and gives its entire curve greater area. Do not equate the numerical peak height with total emitted power or read a wavelength-plot peak as if it were a frequency-plot peak.

Blackbody continuum: peak and area are differentThe two continuous spectra show spectral intensity per unit wavelength against wavelength on common linear axes. The 3000 K peak is at 0.967 μm; the 6000 K peak is at 0.483 μm. The hotter-to-cooler ratio of complete spectrum areas is 16, while the ratio of peak heights is 32.Spectral intensity per unit wavelength (common relative scale)00.5123400.51Vacuum wavelength λ (μm)6000 K = 2T3000 K = T; peak near 0.967 μmHot peak near 0.483 μmFull shaded-area ratio = 16Peak-height ratio = 32Both curves continue beyond this window.
Blackbody continuum: peak and area are different.
Accessible samples of both spectra on the same scale
λ (μm)3000 K spectral intensity6000 K spectral intensity
0.250.00000.2615
0.4830.00691.0000
0.9670.03120.4043
20.01170.0504
40.00160.0044
Peak versus complete area comparison
TemperaturePeak λ (μm)Peak height relative to 3000 KTotal intensity relative to 3000 K
30000.96711
60000.4833216

The vertical scale divides both spectral intensities by the hotter peak height. Shading marks the area under each curve in the displayed interval; the complete area includes the long-wavelength tails beyond 4 μm. The exact total-area ratio 16 follows σT⁴. The 32 peak-height ratio illustrates why one peak height cannot stand in for that area. The construction uses the Planck shape; an AP response uses its qualitative curve and Wien/Stefan–Boltzmann laws, without deriving that shape.

Use absolute temperature and distinguish total from net power

Wien's displacement law is λmax⁡T=b,b=2.90×10−3 m K\lambda_{\max}T=b,\quad b=2.90\times10^{-3}\ \mathrm{m\,K}. A hotter blackbody peaks at shorter wavelength. Use kelvins: temperature ratios in Celsius do not apply.

The total emitted power of an ideal blackbody is P=AσT4P=A\sigma T^4, where σ = 5.67 × 10⁻⁸ W/(m²·K⁴) and A is its emitting surface area. Doubling T at fixed A multiplies P by 16; doubling A at fixed T multiplies P by 2. This is emitted power, not automatically the net energy loss. In an environment a body also absorbs radiation; a simple blackbody net-loss model would subtract the incoming term. The AP comparison must state which power is being used.

Peak and power scale differently

An ideal blackbody has area 0.020 m² and temperature 3000 K. Find peak wavelength and total emitted power; compare with 6000 K at the same area.

  1. λmax = b/T = (2.90 × 10⁻³)/3000 = 9.67 × 10⁻⁷ m = 967 nm.

    Why this step? Wien’s law gives the peak of the wavelength distribution, not a single emitted color.

  2. P = AσT⁴ = (0.020)(5.67 × 10⁻⁸)(3000)⁴ = 9.19 × 10⁴ W.

    Why this step? Emitted power sums over the entire spectrum and the emitting area.

  3. At 6000 K the peak wavelength halves to 483 nm and P increases by 2⁴ = 16 to 1.47 × 10⁶ W.

    Why this step? Temperature ratios control the two laws differently.

Answer and check

967 nm and 9.19 × 10⁴ W at 3000 K; 483 nm and 1.47 × 10⁶ W at 6000 K.

Blackbody continuum: peak and area are differentThe two continuous spectra show spectral intensity per unit wavelength against wavelength on common linear axes. The 3000 K peak is at 0.967 μm; the 6000 K peak is at 0.483 μm. The hotter-to-cooler ratio of complete spectrum areas is 16, while the ratio of peak heights is 32.Spectral intensity per unit wavelength (common relative scale)00.5123400.51Vacuum wavelength λ (μm)6000 K = 2T3000 K = T; peak near 0.967 μmHot peak near 0.483 μmFull shaded-area ratio = 16Peak-height ratio = 32Both curves continue beyond this window.
Blackbody continuum: peak and area are different.
Accessible samples of both spectra on the same scale
λ (μm)3000 K spectral intensity6000 K spectral intensity
0.250.00000.2615
0.4830.00691.0000
0.9670.03120.4043
20.01170.0504
40.00160.0044
Peak versus complete area comparison
TemperaturePeak λ (μm)Peak height relative to 3000 KTotal intensity relative to 3000 K
30000.96711
60000.4833216

The vertical scale divides both spectral intensities by the hotter peak height. Shading marks the area under each curve in the displayed interval; the complete area includes the long-wavelength tails beyond 4 μm. The exact total-area ratio 16 follows σT⁴. The 32 peak-height ratio illustrates why one peak height cannot stand in for that area. The construction uses the Planck shape; an AP response uses its qualitative curve and Wien/Stefan–Boltzmann laws, without deriving that shape.

Try it from memory

Write your answer and reason before opening the worked answer. Your self-assessment is a study decision; it is not an automatically graded score.

Question 1

Two identical-temperature blackbodies have areas A and 3A. Compare their peak wavelength, intensity per wavelength, and total emitted power.

Worked answer and reason

Same peak and same spectral intensity per unit emitting area; the larger body emits three times total power.

Surface area multiplies power but does not alter the temperature-dependent spectrum per area.

Question 2

A graph’s vertical axis is W/(m²·μm). Does its maximum height equal total intensity in W/m²?

Worked answer and reason

No. Sum across wavelength intervals or take the graph’s area to obtain total intensity; the peak height is per unit wavelength.

The units reveal why peak and integrated quantity differ.

JavaScript enables saved drafts and self-assessment. You can always work on paper.

Catch the tempting mistake

A blackbody emits only at its peak wavelength.
It emits a continuous distribution; Wien’s law locates the greatest spectral contribution, not the only wavelength.

Put it to work

Give the physical reason as well as the calculation. The worked solutions are on a separate page.

Scientific calculator workspace

Keep intermediate precision and report units. This calculator supports arithmetic and elementary functions.

Scientific calculator

This calculator requires JavaScript. Use the physics formula sheets and show your working manually.

Calculation is unavailable without JavaScript.

+ − * / ^ ! · pi · e · sqrt · sin, cos, tan · asin, acos, atan · atan2(y,x) · ln, log · abs · exp · hypot(x,y). Use * between factors. Keep units in your written working.

For the teacher
  • Require both peak-position and integrated-area comments on a spectral graph. Do not infer true temperature from an uncalibrated phone photograph’s color.

Unit planning and inquiry guidance →

Source objectives and scope
  • 15.4.A — Describe the electromagnetic radiation emitted by an object due to its temperature.

Suggested skills are teaching guidance. The course applies all science practices across its objectives.

Science references for this teaching
Glossary and deeper reading · 12 refreshers

These editorial refreshers supplement the reading. Definitions and examples are added guidance; original source wording and recorded answers remain in their original context.

  • Wavelength

    Wavelength is the spatial distance between neighboring points at the same phase of a periodic wave. It connects propagation speed and frequency through speed equal to frequency times wavelength. For example, neighboring crests of a sinusoidal water wave are separated by one wavelength.

    Read more: Wavelength in detail →

  • Power

    Power is the rate at which energy is transferred or converted. It is measured in watts, with one watt equal to one joule per second. For example, two motors can lift the same load through the same height but have different average powers if they take different times.

    Read more: Power in detail →

  • Kelvin temperature scale

    The kelvin scale measures thermodynamic temperature from absolute zero. A temperature interval of one kelvin has the same size as one degree Celsius, but their zero points differ. For example, temperature ratios in the ideal gas law must use kelvin values rather than Celsius values.

  • Temperature

    Temperature is a state quantity that determines the direction of net energy transfer through thermal contact. For a classical ideal gas it is proportional to the average translational kinetic energy per particle, rather than to the total energy of the sample. For example, a small hot metal sample can have a higher temperature but less total internal energy than a large cooler sample.

    Read more: Temperature in detail →

  • Electromagnetic wave

    An electromagnetic wave contains oscillating electric and magnetic fields that transport energy. In the plane-wave vacuum model, both fields are perpendicular to each other and to the propagation direction. For example, visible light and radio waves can both travel through empty space.

    Read more: Electromagnetic wave in detail →

  • Thermal radiation

    Thermal radiation is electromagnetic energy emitted by matter because of its temperature. It can transfer energy through a vacuum, and net radiative transfer between ordinary bodies is from hotter to cooler. For example, sunlight warming a surface does not need air to carry the energy across space.

    Read more: Thermal radiation in detail →

  • Emission spectrum

    An emission spectrum shows the frequencies or wavelengths of radiation emitted by a source. An excited dilute gas produces characteristic bright lines associated with allowed energy-level transitions. For example, comparing several observed lines with known element spectra can help identify which atoms are present.

    Read more: Emission spectrum in detail →

  • Emissivity

    Emissivity describes a surface’s thermal-radiation emission compared with an ideal blackbody at the same temperature. It is dimensionless and can depend on wavelength, surface condition, and temperature. For example, two surfaces of equal area at the same temperature can radiate different powers because their emissivities differ.

  • Wave intensity

    Wave intensity is the time-averaged energy-transfer rate per area perpendicular to propagation. It is measured in watts per square meter and differs from total power because area matters. For example, spreading the same sound power over a larger area reduces the intensity there.

    Read more: Wave intensity in detail →

  • Quantization

    Quantization means a quantity can take only certain allowed values in the stated quantum system. Bound-state boundary conditions can restrict energy to discrete levels rather than a continuous range. For example, an electron bound in a hydrogen atom cannot have an arbitrary energy between its allowed levels.

    Read more: Quantization in detail →

  • Frequency

    Frequency is the number of complete repeating cycles per unit time. It is measured in hertz, meaning cycles per second, and is the reciprocal of the period. For example, a vibrating string with a higher frequency produces more cycles each second.

    Read more: Period, frequency, and wavelength →

  • Wien’s displacement law

    Wien’s displacement law relates a blackbody spectrum’s peak wavelength to its kelvin temperature. The peak wavelength is inversely proportional to temperature when the spectrum is expressed per unit wavelength. For example, a hotter blackbody peaks at a shorter wavelength, though it still emits across a broad range.

Search lessons, terms and problems