Blackbody Radiation Calculator

Blackbody Radiation Calculator

Calculate Planck-law spectral radiance at a wavelength, Wien peak wavelength, Stefan-Boltzmann total surface flux, band-integrated flux, emitted power, and observer irradiance for ideal or graybody emitters.

✨Radiation Presets
⚙Inputs
Used in result cards, comparison notes, and print output.
Converted to Kelvin before Planck, Wien, and flux calculations.
Kelvin is recommended for scientific inputs.
The spectral radiance card evaluates Planck law here.
Visible light is roughly 380 to 700 nm.
Planck law is computed internally as W/mÂł/sr.
Used for numerical integration of surface exitance.
The calculator swaps limits if start is greater than end.
Choose a unit that matches both band limits.
Use 1 for an ideal blackbody; graybody output scales by emissivity.
Used to estimate emitted power from surface flux.
Solar surface area means 4 pi Rsun squared.
Used for inverse-square irradiance from total emitted power.
Set 1 AU with solar area to approximate sunlight at Earth.
More samples improve broad-band estimates.
Internal calculation uses full JavaScript precision.
Scientific notation is useful for radiance and power.
📊Results
Spectral radiance 0 W/m²/nm/sr
Wien peak 0 peak wavelength
Total surface flux 0 Stefan-Boltzmann
Band fraction 0 integrated band
🔢Computed Metrics
⚖Comparison Grid
🌌Spectral Sample Table
Wavelength Region Radiance Exitance Photon energy
🔭Reference Blackbodies
Emitter Temperature Wien peak Main region Surface flux
Cosmic microwave background2.725 K1.06 mmMicrowave3.13e-6 W/m²
Room-temperature surface293 K9.89 umThermal infrared419 W/m²
Human skin estimate310 K9.35 umThermal infrared524 W/m²
Molten lava estimate1200 K2.41 umNear infrared117,600 W/m²
Tungsten lamp filament2800 K1.03 umNear infrared3.48 MW/m²
Solar photosphere5772 K502 nmVisible63.2 MW/m²
Blue star surface15000 K193 nmUltraviolet2.87 GW/m²
🌈Wavelength Bands
Band Approx range Useful for Calculator note
Ultraviolet10 to 380 nmHot stars, lampsUse small nm limits and scientific display.
Visible380 to 700 nmSolar-like starsSolar-temperature blackbodies put a strong share here.
Near infrared0.7 to 2.5 umWarm filaments, lavaOften dominates objects near 1000 to 3000 K.
Thermal infrared2.5 to 25 umPeople, rooms, planetsUse micrometers for comfortable input values.
Far infrared25 to 1000 umCold dust, cryogenic surfacesLow temperatures shift the peak into this range.
Microwave1 mm and longerCMB, very cold emittersMillimeter inputs are easier for cosmic background checks.
📐Constants and Formulas
Item Formula or value Meaning Output used
Planck spectral radianceB_lambda = 2hc²/lambda⁾ / (exp(hc/(lambda kT)) - 1)Radiance per wavelength per steradianCard 1 and sample table
Wien displacementlambda_max = 2.897771955e-3 / TPeak wavelength of B_lambdaCard 2
Stefan-Boltzmann fluxF = emissivity x sigma x T⁴Total emitted power per square meterCard 3 and power
Band integrationIntegral of pi x B_lambda dlambdaSurface flux inside selected wavelength bandCard 4 and breakdown
Photon energyE = hc / lambdaEnergy of one photon at sample wavelengthMetric and table
Observer irradianceP / (4 pi d²)Inverse-square irradiance from entered total powerMetric card
🧮Formula Notes
Planck law scopeThe spectral radiance formula here uses wavelength form, B_lambda(T), in SI units. It assumes an ideal blackbody spectrum before the optional emissivity scale is applied.
Exitance versus radianceFor a Lambertian blackbody surface, spectral exitance is pi times spectral radiance. That is why band power integrates pi x B_lambda over wavelength.
Total flux checkThe full wavelength integral of pi x B_lambda equals sigmaT⁴. The band fraction compares the selected integral with that Stefan-Boltzmann total.
Distance estimateObserver irradiance treats the entered surface power as isotropic total emitted power. Extended nearby surfaces need geometry-specific view-factor modeling.
💡Tips
Match the unit to the source.Use nanometers for stars and lamps, micrometers for people and rooms, millimeters for cosmic microwave background work.
Check both peak and band.A blackbody can peak outside a band but still radiate meaningful power inside it, especially at high temperature.
Emissivity is a scale factor here.Real materials can have wavelength-dependent emissivity; this calculator uses one graybody value for a quick estimate.
Use area deliberately.Surface flux is independent of area, but emitted power and distance irradiance both scale directly with the area you enter.

Heat is light. Light is energy in motion within space. Any object at any temperature higher than absolute zero will emit this energy. The formula is all physics, but it’s also something that humans can understand and work with.

That’s what the calculator above does for you: it takes raw physics, and makes it tangible. It tells you what kind of energy a given surface produce, and at what wavelengths. And why? Because you can then take that information and make predictions about thermal properties of whatever material you’re modeling. You don’t have to set up a lab experiment. You could be predicting the behavior of a toaster filament, or a human body, or even a star.

How Heat Works Like Light

Blackbody theory makes these different system seem like they come from the same source. They show us how the visible world connects to the invisible infrared world. We cannot see infrared with our eyes.

These are based on Planck’s law which describes the spectral radiance of an ideal emitter at some particular temperature. Type in 500 nanometers, and it’ll tell you how much light at that wavelength the 5772 Kelvin photosphere emit. And what does this mean?

Well, if you think about it, the sun shouldn’t appear yellow-white, it should just be plain old blue. However, the sun peaks in the green-blue region of the spectrum. That means it looks yellow-white because your eyes integrates all the different wavelengths. The calculator breaks out those wavelengths so you can see where the power lies along electromagnetic spectrum.

That brings us back to Wien’s displacement law which tells you where the maximum emission occurs for an object of a given temperature. That maximum increases with temperature; moving from longer wavelengths towards shorter ones. In other words, a hot object radiates in the UV or maybe the visible range while a cold object give off microwaves or even way-out-in-the-back-of-the-closet far infrared.

The figure on the page puts it all nicely into a reference table that illustrates this as well: the CMB, which has a temperature of only 2.73 Kelvins, has a peak at 1.06 millimeters, which is in the far microwave radiation range. Why does space look so dark to your eye but glow away merrily in radio telescope pictures? Because they’re seeing the same thing; the change is just smooth and predictable. You don’t have to memorize the curve; you only need to know temperature. Now we are getting somewhere.

That’s a lot of energy. How much? The Stefan-Boltzmann law gives us a way to measure all of it. Total flux scales by the fourth power of the temperature. So, a little bit more heat produces an enormous leap in radiation. Double the temperature and you have sixteen times the power! This is why stars glow as bright as they do. It’s also why engineering problems involving heat are tricky.

The tool provides the total surface flux. Once you calculate that, you have a starting point for understanding how much energy to expect. From there, you can add a factor for emissivity if you’re working with a graybody (not a perfect blackbody). In reality, most things aren’t perfect emitters. Tweaking this parameter will adjust the model to reflect reality.

You split up the spectrum and integrate the bands using band integration. Suppose that you wanted to calculate how much light is between 380-700 nm, which is useful for estimating photosynthetic active radiation or solar panel efficiency. If you are sizing a solar panel or looking at photosynthetic active radiation then this may be relevant. For this case, the calculator integrates Planck’s function across this wavelength range. It returns a fraction of total.

Is a heat source more suited to heating than lighting? That can sometimes make a big difference when designing something.

Distance matters. Distance matters, because energy radiates. As it travels, it spreads out. How? The inverse-square law means energy decreases in proportion to the square of distance. Want an example? Stand close to a fire and you will feel warmth, but move a few feet away and you will feel cold. That’s the inverse-square law in action.

The same geometry applies to your input. It links the source to the observer. The link is the physical picture that completes the bridge from emission to reception.

There are common errors too. Failing to get the units straight. They use meters instead of nanometers or Celsius instead of Kelvin. Confusing them and the formulas won’t work. Another mistake is overlooking emissivity. If you assume something is a perfect blackbody, you’ll be overestimating. Surfaces don’t just absorb all light. Some is reflected. Your model should account for that. It’s an honest way to model.

Blackbody radiation: The invisible link between light and heat explained. Convert temperature to spectrum. The distance affects the intensity. This works through complex math and simple intuition.

The hotter it gets, the bluer it gets. The closer it is, the more intense it becomes. Whether you’re talking thermal imaging or stellar evolution, these rules apply. Heat is light and light is heat.

Blackbody Radiation Calculator