The convective heat transfer coefficient h quantifies how effectively a fluid moves heat across a surface. This calculator computes h from a measured heat transfer rate, surface area, and temperature difference, or solves for any one of the four quantities in Q = hAΔT given the other three.

How the calculator works

Newton's law of cooling states that the rate of convective heat transfer Q is proportional to the surface area A and the temperature difference ΔT between the surface and the fluid, with the constant of proportionality being the heat transfer coefficient h: Q = hAΔT. Rearranged, h = Q/(AΔT) lets you back out the coefficient from a measured or specified heat rate. The same equation, rearranged differently, solves for heat rate, area, or temperature difference when the other three values are known.

Inputs and what they mean

Heat transfer rate (Q) is the total thermal power moving across the surface, in watts. Surface area (A) is the area in contact with the fluid, in square meters, and must be greater than zero. Temperature difference (ΔT) is the gap between the surface and the fluid temperature, in kelvin or degrees Celsius — since it is a difference, the two scales give the same number, but it must not be zero or the coefficient is undefined. The resulting coefficient h is expressed in watts per square meter-kelvin.

Limits and edge cases

This calculator assumes a single, uniform coefficient over the whole surface and a fixed temperature difference — real convective flows often have a coefficient that varies with fluid velocity, surface geometry, and whether the flow is laminar or turbulent, and detailed correlations (like the Nusselt number relations) are needed to predict h from first principles rather than back-calculate it. It also does not separate forced convection (fan- or pump-driven flow) from natural convection (buoyancy-driven flow), which typically produce very different coefficients for the same fluid, nor does it account for radiative or conductive heat transfer occurring alongside convection.