Pitot Tube Airspeed
Also known as: Pitot-Static Equation · Dynamic Pressure Speed
Bring the moving air to a dead stop at the tube's nose and all its kinetic energy turns into extra pressure. The size of that extra (dynamic) pressure tells you how fast the air was going.
Air streams toward a pitot tube and stagnates at the nose; a manometer column rises with the dynamic pressure and the computed airspeed updates as you drag the speed slider.
Equivalent forms
A speedometer with no moving parts — just a hole facing the wind and Bernoulli.
Unit systems
Where it holds
Dimensional analysis
[\sqrt{(p_0-p)/\\rho }] = \ = \ (velocity)
Pitot built an L-shaped open tube to measure the speed of the river Seine, finding flow slower at depth than engineers assumed. Henry Darcy later refined the design; the pitot-static tube is now the primary airspeed sensor on virtually every aircraft.
Every airliner reads its speed from a bent tube and Bernoulli's equation — how?
An aircraft pitot tube measures a pressure difference (stagnation minus static) of 2000 Pa in air of density 1.2 kg/m³. What airspeed does that imply?
- Primary aircraft airspeed indication
- Wind-tunnel and HVAC duct flow measurement
- Racing-car and marine speed sensing
- Industrial gas-flow metering
- The tube measures velocity directly — it measures a pressure difference that depends on density too
- Indicated airspeed equals true airspeed — they diverge as air thins with altitude
- Blockage just zeroes the reading — a frozen or blocked pitot can give dangerously wrong, sometimes increasing, indications (a known cause of accidents)
Limiting cases
What if…
The reference pressure freezes at the old value, so the indicated speed reads wrong as altitude changes — a classic instrument failure mode.
Lower density yields a smaller pressure difference, so indicated airspeed drops even though true airspeed is unchanged.
Airspeed from a pitot reading
- p 0:
- 103325
- p:
- 101325
- \rho:
- 1.2
- Dynamic pressure
- — a typical small-aircraft cruise speed