Enter the Stefan-Boltzmann constant and the thermodynamic temperature into the calculator to determine the total radiation energy emitted per unit surface area of a black body in unit time. This calculator can also evaluate any of the variables given the others are known.

Stefan’s Law Calculator

Enter one value to calculate the other


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Stefan’s Law Formula

Stefan’s Law, more precisely the Stefan-Boltzmann law, relates the thermal radiation emitted by an ideal black body to its absolute temperature. The calculator returns emitted radiant power per unit surface area, so the result is an energy flux rather than the total power of an entire object.

E = \sigma T^4

If you need to solve for temperature instead of emitted radiation, the equation is rearranged to:

T = \left(\frac{E}{\sigma}\right)^{1/4}

For real materials that are not perfect black bodies, emissivity is often included:

E = \varepsilon \sigma T^4

Variable Definitions

Symbol Description Common Units
E Total radiation energy emitted per unit surface area per unit time (radiant exitance) W/m² or BTU/hr·ft²
σ Stefan-Boltzmann constant 5.670374419 × 10-8 W·m-2·K-4
T Absolute temperature of the emitting surface K
ε Emissivity of a real surface Dimensionless, from 0 to 1

How to Use the Calculator

  1. Choose which value you want to solve for: emitted radiation or temperature.
  2. Enter the known value in the selected units.
  3. If temperature is entered in °C or °F, remember the law itself uses absolute temperature, so the calculator converts internally to Kelvin.
  4. Read the result as emission from each unit of surface area. If you need total power, multiply by the object’s area.

Temperature Must Be Absolute

The fourth-power relationship only works correctly with absolute temperature. That means Kelvin must be used in the formula even if the input is entered in Celsius or Fahrenheit.

T_K = T_{^\circ C} + 273.15
T_K = \frac{5}{9}\left(T_{^\circ F} - 32\right) + 273.15

Why the Result Changes So Quickly

Radiative emission is proportional to the fourth power of temperature. This makes Stefan’s Law extremely sensitive to temperature changes. A modest rise in temperature can produce a much larger rise in emitted energy.

\frac{E_2}{E_1} = \left(\frac{T_2}{T_1}\right)^4

For example, if the absolute temperature doubles, the emitted radiation increases by a factor of 16.

Example Calculation

For an ideal black body at 300 K:

E = \sigma (300)^4
E \approx 459.3\ \mathrm{W/m^2}

This means each square meter of surface emits about 459.3 watts of thermal radiation.

From Emission Per Area to Total Power

The calculator result is usually expressed per unit area. If you need the total radiated power from an object with surface area A, multiply the emitted flux by area:

P = E A = \sigma A T^4

This is useful for estimating the total radiative output of heaters, furnaces, stars, hot plates, and other radiating surfaces.

Practical Engineering Note

Stefan’s Law in its basic form assumes a perfect black body. Real surfaces emit less than that ideal unless their emissivity is very close to 1. Polished metals usually have much lower emissivity than dark, matte, or oxidized surfaces. When emissivity matters, use the generalized form with ε.

Net Radiation to Surroundings

If you are analyzing heat loss instead of total emitted radiation alone, the surroundings also matter. A common net-radiation form is:

q = \varepsilon \sigma \left(T_s^4 - T_{sur}^4\right)

This version is often used in heat transfer problems where a hot surface radiates to a cooler environment.

Common Mistakes to Avoid

  • Using Celsius or Fahrenheit directly in the fourth-power equation instead of converting to Kelvin first.
  • Confusing emitted energy per unit area with total power from the whole object.
  • Assuming all materials behave like perfect black bodies.
  • For heat-loss problems, forgetting that surrounding temperature affects net radiation.

Where Stefan’s Law Is Used

  • Thermal engineering and furnace design
  • Infrared sensing and thermal imaging
  • Astrophysics and stellar radiation estimates
  • Climate and atmospheric radiation models
  • High-temperature material and surface analysis