Combined Convection and Radiation Coefficient

Radiation is a fourth-power law, but T₁⁴ − T₂⁴ factors exactly into (T₁ − T₂)(T₁ + T₂)(T₁² + T₂²), so over a modest temperature range you can hide everything but the linear ΔT inside an equivalent coefficient $h_r = \varepsilon\sigma(T_s + T_{\mathrm{sur}})(T_s^{2} + T_{\mathrm{sur}}^{2})$. Add it to the convective film and a single $h_t$ drives the whole surface with plain old Q̇ = $h_t A \Delta T$, which is exactly what makes building-envelope and insulation software tractable.

The size of the radiation term surprises people. A painted surface (ε = 0.9) at 350 K facing 293 K surroundings has $h_r$ = 6.8 W/(m²·K), larger than the 5 W/(m²·K) of still-air natural convection beside it, giving $h_t$ = 11.8. That is why a bare hot pipe in a still basement loses more than half its heat by radiation, and why a low-emissivity foil wrap, ε ≈ 0.05, kills that channel almost completely while doing nothing about convection. The two traps: $h_r$ depends on both temperatures, so it is not a constant and must be recomputed if the surface moves far; and the surroundings temperature is the temperature of the walls seeing the surface, not the air temperature, which on a clear night can be 20 K colder than the air and is why cars frost over at 4 °C.