This calculator finds the constant speed a falling object eventually reaches once air resistance grows large enough to balance its weight. It's the same physics behind skydiving speeds, raindrop sizes, and why a feather and a bowling ball fall very differently in air (but identically in a vacuum).
How the Terminal Velocity Calculator works
As an object falls, gravity accelerates it downward while air resistance (drag) pushes back, growing stronger the faster it goes — drag force scales with velocity squared. Eventually drag force exactly equals the object's weight, acceleration drops to zero, and the object falls at a constant speed: its terminal velocity. The calculator solves v = √(2mg / (ρ·A·Cd)) directly from Newton's second law at that equilibrium point, using standard gravity g = 9.80665 m/s².
Inputs and what they mean
Mass (kg) is the total weight of the falling object, including any gear. Cross-sectional area (m²) is how much surface the object presents to the oncoming air — a spread-eagle skydiver presents far more area than the same person diving head-down. Drag coefficient is a dimensionless shape factor: streamlined shapes have low values (0.04-0.3), flat or irregular shapes are closer to 1.0-1.3, and a deployed parachute canopy is typically 1.3-1.5. Air density (kg/m³) defaults to 1.225, the sea-level standard, but drops at altitude — thinner air means less drag and a higher terminal velocity for the same object.
Limits and edge cases
This formula assumes a constant drag coefficient and steady, low-turbulence airflow, which is a good approximation for most everyday falling objects but breaks down at very high speeds (transonic and supersonic regimes, where drag behaves differently) or for objects that tumble and change orientation mid-fall. It also assumes the object starts from rest and has enough distance to actually reach terminal velocity — a skydiver typically needs about 12 seconds and 450-460 meters of fall to get there. Air density inputs should reflect the altitude and conditions of the fall, not just sea level, for the most accurate result.