Forced Convection Heat Transfer

Q = h × A × ΔT

Calculator

Result

Formula

Q = h × A × ΔT

Description

Newton's law of cooling describes convective heat transfer from a surface to a moving fluid (air). The convection coefficient h depends on the fluid velocity, fluid properties, and surface geometry. Forced convection (using fans) dramatically increases h compared to natural convection, enabling much higher power dissipation from the same heatsink. This formula is fundamental to heatsink design, enclosure thermal analysis, and cooling system sizing for electronics.

Variables

  • Q — Heat transfer rate (W)
  • h — Convection heat transfer coefficient (W/(m²·°C))
  • A — Surface area exposed to airflow (m²)
  • ΔT — Temperature difference between surface and ambient air (°C)

Practical Notes

Typical h values: natural convection in air 5-25 W/(m²·°C), forced convection in air 25-250 W/(m²·°C), liquid cooling 100-20000 W/(m²·°C). Doubling airflow velocity increases h by roughly 40-50%. Fin spacing must account for boundary layer thickness to avoid diminished returns from closely spaced fins.

Need more features?

Save calculations, import telemetry data, simulate battery discharge, and collaborate with your team.

Try the App