Heat Transfer Coefficient Calculator
Back-calculate a heat-transfer coefficient in W/(m²·K) from a measured heat rate, the area it crosses and the temperature difference driving it.
Heat Transfer Coefficient Calculator
Background.
Stand in a breeze on a cool day and you lose heat faster than in still air at the same temperature. That difference, how readily heat crosses between a surface and a fluid for each degree of temperature gap, is what a heat-transfer coefficient measures. Still air is a poor carrier: the typical-values table in Incropera's heat-transfer textbook puts free convection in gases at 2 to 25 W/(m²·K). Blow the air and the range becomes 25 to 250; pump a liquid past the surface and it runs from 100 to 20,000; boiling or condensing fluids reach 2,500 to 100,000.
Predicting a coefficient from first principles is hard. Correlations for each geometry and flow are approximate, so engineers often work the other way round and measure: supply a known heat rate, measure the area and the temperature difference, and divide. That back-calculation is what happens here.
The result is an effective coefficient. It contains everything that happened between the two temperatures you measured. Across a heated panel in a room, that includes radiation as well as convection. Across a heat-exchanger tube, it includes both fluid films, the metal wall and any scale or deposit, which makes it an overall U value rather than a single film coefficient. Which of these you have depends entirely on where the temperatures were taken, and the arithmetic cannot tell them apart.
That is also what makes it a good diagnostic. An exchanger whose measured coefficient drifts down month after month is fouling, and plotting the figure over time shows when cleaning will pay for itself. A test rig that returns a value far outside the expected range more often has a misplaced thermocouple or an uncounted heat loss than new physics.
What is heat transfer coefficient calculator?
A heat-transfer coefficient is the rate of heat flow per unit area per kelvin of temperature difference, in watts per square metre per kelvin, W/(m²·K). A convection coefficient h describes one surface and the fluid moving past it; an overall coefficient U describes the full path through a wall or exchanger from one fluid to another. Both share the unit and the defining equation, and the reciprocal, 1/h or 1/U, is a thermal resistance per unit area in m²·K/W.
How to use this calculator.
- Enter the heat-transfer rate in watts, measured once conditions are steady. For an electric heater it is the power drawn; for a fluid stream it is mass flow × specific heat × that stream's temperature change.
- Enter the area heat actually crosses, in square metres. For a tube, choose the inside or the outside surface and stick with it, because the coefficient changes with that choice.
- Enter the temperature difference in kelvin; a difference in °C is the same number, and one in °F should be divided by 1.8. For a surface in a fluid, use surface temperature minus bulk fluid temperature; for a heat exchanger, use the log-mean temperature difference.
- Compare the result with the range expected for your situation, remembering that it includes radiation and any other path between your two measuring points.
The formula.
h = Q̇ ÷ (A × ΔT), where Q̇ is the heat-transfer rate in watts, A the area in square metres and ΔT the temperature difference in kelvin. It is Newton's law of cooling, Q̇ = h × A × ΔT, rearranged to give the coefficient. The coefficient rises in direct proportion to the heat rate and falls in inverse proportion to both area and temperature difference, so a 10% error in any one input becomes an error of roughly 9 to 10% in h. The temperature difference is usually the weakest link: with only 10 K between surface and fluid, a thermocouple reading one degree off shifts the coefficient by about 10%. All three inputs must be positive. Nothing here predicts h from fluid properties or flow speed; correlations built on Reynolds, Prandtl and Nusselt numbers do that, and measured coefficients are what those correlations are tested against. The result is rounded to 12 significant figures.
A worked example.
An electrically heated panel draws 1,500 W at steady state, has 5 m² of surface and sits 20 K warmer than the surrounding air. The area times the temperature difference is 5 × 20 = 100 m²·K, and 1,500 ÷ 100 = 15 W/(m²·K). That falls inside the 2 to 25 W/(m²·K) typical of free convection in gases, which suits a panel in still room air, but the measured figure also carries radiation. For a high-emissivity surface (ε = 0.9) near 300 K, the linearised radiation coefficient 4εσT³ comes to about 5.51 W/(m²·K), leaving roughly 9.49 for convection itself. Had the same 1,500 W held the panel only 10 K above the air, the coefficient would be 30 W/(m²·K), a sign of a draught or fan.
Frequently asked questions.
Have I measured a convection coefficient h or an overall U value?
How much does it matter which temperature difference I use for a heat exchanger?
My result seems high for still air. What could be inflating it?
How do I convert W/(m²·K) to Btu per hour per square foot per °F?
Why would a measured coefficient fall over time?
How does the coefficient relate to an R-value?
References& sources.
- [1]Incropera et al., Fundamentals of Heat and Mass Transfer, 8th ed. (PRINT).
- [2]OpenStax, University Physics Volume 2, section 1.6, Mechanisms of Heat Transfer.
- [3]BIPM, The International System of Units (SI Brochure), 9th ed., version 3.01, coherent derived units and quantity equations.
How this page was produced
- Published by
- Quanta Calculator
- Overseen by
- Daniel, Quanta Calculator Researcher
- Primary sources
- 3 cited below
- Method
- h = Q̇ / (AΔT)
- Published
- Last verified
Built with AI assistance and verified by automated tests against the cited sources — every worked example on this page is computed by the same code that runs the calculator. How we build and check calculators.
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