Radiation Heat Transfer Calculator.

Heat crossing empty space, needing no medium at all. Near room temperature it carries about as much as free convection in still air; the fourth-power law makes it dominant in a furnace, and the curve beside the stage shows where it pulls ahead.

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Radiation — the Stefan–Boltzmann Law

Radiation — ε = 0.8 · F = 1 · net 18.21 kWhotcoldT₁ = 800 KNET EMITTERA = 1 m²T₂ = 300 KNET RECEIVERnet exchange Q = εσFA(T₁⁴ − T₂⁴)Wave count tracks the magnitude of Q; both surfaces radiate at all times
200650110015502000-294.9 W181.14 kW362.57 kW544.01 kW725.44 kWT₁, the hot surface (K)net QQ rises as the FOURTH power of T₁

Heat rate Q

18.21 kW

Thermal resistance R

0.02745 K/W

Heat flux q

18,213 W/m²

Driving ΔT

500 K

Radiative h_r

36.43 W/m²·K

Emitted at T₁ (εσT⁴)

18,581 W/m²

Mode

Radiation

Formula

Q = εσFA(T₁⁴ − T₂⁴)

No warnings — every assumption behind these numbers holds for this set-up.

The arithmetic, with your numbers in it

T₁⁴ − T₂⁴ = 4.10e+11 − 8.10e+9 = 4.02e+11 K⁴

h_r = εσF(T₁+T₂)(T₁²+T₂²) = 36.43 W/m²·K — exact, not a linearisation

R = 1 / (h_r·A) = 0.02745 K/W

Q = ΔT / R = 500 / 0.02745 = 18213.2 W

check: εσFA(T₁⁴−T₂⁴) = 18213.2 W — the same number

Presets

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Surface

Radiation at a glance: the Stefan–Boltzmann Law

Across a vacuum. Modest when cool, unbeatable when hot, because of T⁴. The law is Q = εσFA(T₁⁴ − T₂⁴), and as a thermal resistance it reads R = 1 / (h_r·A), so the heat rate is always Q = ΔT / R.

At the instrument's opening set-up it gives a heat rate of 18.21 kW through a resistance of 0.02745 K/W, a flux of 18,213 W/m² and a radiative h_r of 36.43 W/m²·K. Open The arithmetic, with your numbers in it above to see each of those worked through with the values on the sliders.

Where radiation comes from

Every object above absolute zero radiates. The Stefan–Boltzmann law says the emissive power of a blackbody goes as the fourth power of absolute temperature, and for a real surface exchanging with another the net flow is Q = εσF A (T₁⁴ − T₂⁴), where ε is the emissivity, σ is 5.670374419 × 10⁻⁸ W/m²·K⁴ and F is the view factor describing how much of one surface the other can actually see.

The fourth power is the whole character of the mode. Against a 20 °C background, a surface at 350 K radiates about 360 W per square metre at ε = 0.8; take the same surface to 1200 K and it radiates about 93,744 W. The temperature went up by a factor of 3.4 and the heat went up by a factor of roughly 260. This is why radiation is a rounding error in a centrally heated room and the dominant term inside a furnace.

Two absolute temperatures are required, in kelvin or degrees Rankine. Feeding celsius into a fourth power is not a small error — it is the single most common mistake in the subject, and it does not merely shift the answer, it changes it by orders of magnitude.

Where an engineer meets it

Radiation is the only mode that crosses a vacuum, which makes it the entire thermal design problem for a spacecraft and the reason a vacuum flask works. It is also why a clear night can put frost on a car while the air temperature never drops below zero: the roof is radiating to a sky that behaves as though it were at about 230 K, and it loses more that way than convection can replace.

Emissivity is a surface property, not a bulk one, and it is where most of the engineering leverage sits. Polished aluminium sits near 0.04 and anodised aluminium near 0.82 — the same metal, a factor of twenty apart, decided by a few microns of oxide. Low-emissivity window coatings, radiant barriers in lofts and the silvering inside a flask are all the same idea applied deliberately.

The mistakes that cost marks

  • Writing the law as εσA(ΔT)⁴. The difference of fourth powers is not the fourth power of the difference, and the two are not close. With T₁ = 800 K and T₂ = 300 K, T₁⁴ − T₂⁴ is about 3.8 × 10¹¹ while (ΔT)⁴ is about 6.3 × 10¹⁰ — a factor of six. The reference tool this page was built against prints exactly this on its readout chip.
  • Using celsius. The fourth power requires an absolute scale, so temperatures must be in kelvin or degrees Rankine. This page only ever offers you absolute units in radiation mode, which removes the trap rather than warning about it.
  • Ignoring the view factor. Two surfaces that cannot see each other exchange nothing, however hot they are. Setting F = 1 assumes each surface sees only the other and nothing else, which is true for a small body inside a large enclosure and false for almost every other arrangement.

Radiation — common questions

What is the Stefan-Boltzmann law?

The Stefan-Boltzmann law gives the thermal radiation emitted by a surface as proportional to the fourth power of its absolute temperature. For net exchange between two surfaces, Q = εσFA(T₁⁴ − T₂⁴), where ε is emissivity, σ = 5.670374419 × 10⁻⁸ W/m²·K⁴, F is the view factor and temperatures are absolute. Near room temperature a black surface exchanges about 6 W/m²·K (4σT³ at 300 K), the same order as free convection in air; the fourth-power dependence is what makes radiation dominant in a furnace.

Why must radiation temperatures be in kelvin?

Because the law depends on the fourth power of absolute temperature, and celsius is not an absolute scale — its zero is arbitrary. Using 100 °C instead of 373 K does not shift the answer slightly; it changes it by many orders of magnitude, and the sign can come out wrong as well. This calculator only offers kelvin and degrees Rankine in radiation mode so the mistake cannot be made.

What is emissivity and what affects it?

Emissivity is the fraction of blackbody radiation a real surface actually emits, between 0 and 1. It is a property of the surface rather than the bulk material, so the finish matters far more than the substance: polished aluminium is about 0.04 while anodised aluminium is about 0.82. Most non-metals, whatever their visible colour, sit between 0.85 and 0.95 — white paint is nearly black in the infrared.

At what temperature does radiation start to dominate?

There is no single crossover, because it depends on how strong the convection is, but the fourth power makes the trend sharp. At ε = 0.8 against a 20 °C background, a surface at 350 K radiates roughly 360 W/m², which a light breeze would beat easily. At 1200 K the same surface radiates about 93,744 W/m², which no practical air flow can match. In round terms, above about 600 °C radiation is usually the leading term.

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