Terminal Velocity Calculator
Calculate terminal velocity from mass, area, drag coefficient, and fluid density. Solve for any variable. Includes skydiver, sphere, and raindrop presets.
Terminal Velocity Scaling
| Change | Terminal Velocity Effect | Reason |
|---|---|---|
| Mass doubles | Increases by √2 | Velocity scales with square root of mass |
| Area doubles | Decreases by √2 | More drag area |
| Drag coefficient quadruples | Halves | Velocity scales with inverse square root of drag |
| Air density doubles | Decreases by √2 | Denser fluid creates more drag |
| Mass quadruples | Doubles | Velocity scales with square root of mass |
Frequently Asked Questions about the Terminal Velocity Calculator
What is terminal velocity?
Terminal velocity is the constant speed a falling object reaches when air drag balances gravity. From that point on, there is no net force, so no further acceleration. For a skydiver in a spread-eagle position, that is roughly 53 m/s (120 mph).
What is the terminal velocity formula?
v = sqrt(2 m g / (rho x C_d x A)), where m is mass, g is 9.81 m/s^2, rho is fluid density, C_d is drag coefficient, and A is cross-sectional area. Doubling mass increases v by only sqrt(2), so terminal velocity grows slowly with size.
Why does a heavier skydiver fall faster?
More mass means more gravity pulling down without much change in cross-section or drag, so the equilibrium speed is higher. A 100 kg skydiver tops out around 60 m/s belly-down; a 60 kg skydiver tops out around 47 m/s in the same posture.
What drag coefficient should I use?
The presets use about 1.0 for a belly-down skydiver, 0.7 for a head-down skydiver, 0.47 for a sphere, and 0.5 for a large raindrop. Drag coefficient changes with shape, orientation, surface, and flow conditions. For engineering work, use data or testing for your specific geometry.
Does terminal velocity exist in vacuum?
No. Without a fluid there is no drag force to balance gravity, so this terminal-velocity model does not apply. In a uniform-field approximation acceleration is treated as constant, but a real gravitational field changes with position. The Moon demonstration showed that objects fall together when air resistance is negligible.
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