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Fluid Mechanics

Dynamic pressure

Pressure associated with a moving fluid.

Ref
FLU-10
Rev
v1
Field
Fluid Mechanics
Result
q [Pa]

ρ is the density of the fluid and v its speed relative to the body. q is the pressure that would be recovered if the flow were brought to rest, and it sets the scale of aerodynamic forces: lift and drag are q times an area times a coefficient. In flow with total pressure p₀ and static pressure p, q = p₀ − p.

Pressure associated with a moving fluid. It sets the scale of aerodynamic forces.

Calculator

Solve for
Pa
kg/m³
0.012,000
m/s
0.12,000
  • Dynamic pressure at twice the speed24,500 Pa
  • Speed in km/h360 km/h

What drives the result

Each variable is moved across its typical range while the others stay at the values above. The longest bar is the key driver.

Dynamic pressure (Pa) current value 6,125 Pa
ρFluid densityKey driver
501e7
vSpeed
0.006132,450,000
  • At 100 m/s (360 km/h) at sea level q is 6.1 kPa, about 6 % of atmospheric pressure. At 200 m/s it is 24.5 kPa, four times as much.
  • Aircraft structures are limited by q rather than by speed alone, because the loads follow q. A fast, high flight can have the same q as a slow, low one.
Chart data as tables

Ranked variables

VariableTypical rangeLowest resultHighest resultSwing (Pa)Local stepChange in result
ρ Fluid density0.01 to 2,000 kg/m³501e710,000,000+10%+10 %
v Speed0.1 to 2,000 m/s0.0061252,450,0002,450,000+10%+21 %

Sweep of Speed

Speed (m/s)Dynamic pressure (Pa)
0.10.006125
0.34480.07284
1.1890.8662
4.10110.3
14.14122.5
48.771,457
168.217,320
580206,000
2,0002,450,000

Sweep one variable

Dynamic pressure (Pa)Hover, touch, or use the arrow keys on the chart
0500k1M1.5M2M2.5M 0.11101001000 Speed (m/s), log scale now 6,125

Variables and how each one contributes

q

Dynamic pressure

Result · Pa

What the equation gives you. Everything else feeds it.

ρ

Fluid density

kg/m³ · typical 0.01 to 2,000

The density of the fluid, in kg/m³ (1.225 for sea-level air at 15 °C). Directly proportional: air at altitude is thinner, so the same speed gives a lower q. Density falls by roughly 10 % per kilometre near sea level.

v

Speed

m/s · typical 0.1 to 2,000

The speed of the flow relative to the body. Squared: doubling the speed quadruples q. A 10 % rise in v raises q by 21 %.

Worked example with the values above

  1. Square the speed: v² = (100)² = 10,000 m²/s².
  2. Multiply by half the density: ½ × 1.225 × 10,000.
  3. q = 6,125 Pa, which is 6.125 kPa.

Assumptions and limits

  • Incompressible flow: valid for air below about Mach 0.3, where the error in q is under 2 %.
  • A uniform, steady stream at a known density.

Common mistakes

  • Entering the speed in km/h.
  • Leaving out the factor ½.

Statistics and uncertainty

q ∝ ρ v², so a 1 % error in speed becomes 2 % in q, while 1 % in density is 1 %. Air density depends on altitude, temperature and humidity, and is usually the least well known input.

Where it is used

  • Aerodynamic loads on a vehicle at a given speed and altitude.
  • Dynamic pressure in a wind-tunnel or flight test.

Maths you need

  • Kinetic energy: ½mv²
  • Pressure: force per unit area

Related formulas

Practise this formula