Mach Number Calculator

Calculate Mach number from velocity and altitude using the International Standard Atmosphere model. Includes flow regime classification, isentropic relations, and altitude comparison table.

ms
m
Mach Number
0.8348
Transonic
Speed of Sound
299.47 m/s
At -50.0°C
Flow Regime
Transonic
No shock waves
Mach Angle
N/A (subsonic)
sin⁻¹(1/M) — half-angle of Mach cone
Stagnation Temperature
-18.9°C
Ratio T₀/T = 1.1394
Stag. Pressure Ratio
1.5789
p₀/p (isentropic)
Density Ratio
1.3857
ρ₀/ρ (isentropic)
True Airspeed
250.00 m/s
900.0 km/h

Mach Meter

0
6+
Incomp.SubsonicTransonicSupersonicHypersonic

Flow Regimes

RegimeMach RangePhysical Effects
Incompressible< 0.3No compressibility effects
Subsonic0.3 – 0.8Mild compressibility, no shocks
Transonic0.8 – 1.2Mixed sub/supersonic, normal shocks
Supersonic1.2 – 5.0Oblique shocks, expansion fans
Hypersonic> 5.0Strong heating, dissociation

Speed of Sound vs Altitude

Altitude (m)Temp (°C)Speed of Sound (m/s)Mach at your speed
015.0340.30.735
2,0002.0332.50.752
5,000-17.5320.50.780
8,000-37.0308.10.812
10,000-50.0299.50.835
12,000-56.5295.10.847
15,000-56.5295.10.847
20,000-56.5295.10.847
25,000-51.5298.50.838
30,000-46.5301.80.828
Planning notes, formulas, and examples

About the Mach Number Calculator

The Mach number is the ratio of an object's speed to the local speed of sound. Named after Austrian physicist Ernst Mach, it is the single most important parameter in compressible aerodynamics, determining whether a flow is subsonic (M < 1), transonic (0.8 < M < 1.2), supersonic (1.2 < M < 5), or hypersonic (M > 5). Each regime brings qualitatively different physics: subsonic flows behave smoothly, while supersonic flows generate shock waves and expansion fans that fundamentally alter drag, lift, and heat transfer characteristics.

The speed of sound depends on the medium's temperature, not altitude directly. In air, a = √(γRT) where γ = 1.4 for diatomic gases, R = 287.058 J/(kg·K), and T is the absolute temperature. Because temperature decreases with altitude in the troposphere (about 6.5°C per kilometer), the speed of sound drops from 340 m/s at sea level to about 295 m/s at the tropopause (11 km). In the lower stratosphere (11–20 km), temperature is nearly constant at −56.5°C, so the speed of sound remains at about 295 m/s.

This Mach number calculator uses the International Standard Atmosphere (ISA) to compute the local speed of sound from altitude, then determines the Mach number and flow regime. It also calculates isentropic stagnation relations — the temperature, pressure, and density ratios that a fluid element would experience if brought to rest — which are critical for designing supersonic inlets, nozzles, and wind tunnels.

When This Page Helps

Mach number is the quickest way to compare a flow speed against the local acoustic limit, which is why it matters for aircraft performance, inlet design, wind-tunnel work, and high-speed vehicle testing. This calculator uses the ISA temperature profile so you can see how altitude changes the speed of sound and immediately interpret the flow regime, cone angle, and stagnation ratios.

How to Use the Inputs

  1. Select a preset aircraft scenario or enter custom velocity and altitude.
  2. Choose the temperature mode: auto (standard atmosphere) or custom.
  3. Select your preferred speed and altitude units.
  4. Enter the velocity of the object.
  5. Enter the altitude (auto mode) or ambient temperature (custom mode).
  6. Review the Mach number, flow regime, Mach angle, and isentropic relations.
  7. Compare speed of sound across altitudes in the reference table.
Formula used
Mach Number: M = v / a. Speed of sound: a = √(γRT). ISA temperature: T = 288.15 − 0.0065·h (troposphere, h ≤ 11 km). Mach cone half-angle: μ = sin⁻¹(1/M) for M > 1. Stagnation temperature ratio: T₀/T = 1 + (γ−1)/2 · M². Stagnation pressure: p₀/p = (T₀/T)^(γ/(γ−1)).

Example Calculation

Result: Mach 0.8376 — Transonic regime

At 10,000 m, ISA temp = 288.15 − 65 = 223.15 K. Speed of sound = √(1.4 × 287.058 × 223.15) = 298.5 m/s. Mach = 250/298.5 = 0.8376. This is in the transonic regime where local supersonic pockets begin forming over wing surfaces.

Tips & Best Practices

  • Commercial jets cruise around Mach 0.78–0.85 to stay below the drag divergence Mach number.
  • Concorde cruised at Mach 2.04 at 60,000 ft, where air temp is about −57°C and speed of sound is 295 m/s.
  • In a wind tunnel, Mach number is set by the nozzle area ratio, not fan speed.
  • Stagnation temperature at Mach 3 is 2.8× ambient — a leading edge at −57°C ambient reaches 345°C.
  • Indicated airspeed (IAS) differs from true airspeed (TAS); Mach number uses TAS.
  • The critical Mach number of an airfoil is the freestream M at which local flow first reaches Mach 1.

The International Standard Atmosphere

The ISA defines standard temperature, pressure, and density profiles from sea level to 86 km. Key layers:

| Layer | Altitude | Lapse Rate | Base Temp | |---|---|---|---| | Troposphere | 0–11 km | −6.5°C/km | 15°C | | Tropopause | 11–20 km | 0°C/km | −56.5°C | | Stratosphere | 20–32 km | +1°C/km | −56.5°C | | Upper strato. | 32–47 km | +2.8°C/km | −44.5°C |

Notable Mach Numbers in History

| Vehicle | Year | Mach | Notes | |---|---|---|---| | Bell X-1 (Chuck Yeager) | 1947 | 1.06 | First piloted supersonic flight | | Concorde | 1976 | 2.04 | Supersonic commercial service | | SR-71 Blackbird | 1976 | 3.32 | Fastest air-breathing jet | | X-15 | 1967 | 6.7 | Hypersonic research aircraft | | Space Shuttle | 1981 | ~25 | Orbital reentry |

Compressibility Effects Summary

Below Mach 0.3, air behaves as essentially incompressible and density changes are negligible. Between 0.3 and 0.8, compressibility corrections (Prandtl-Glauert) become needed. Above Mach 0.8, shock waves begin forming on wing surfaces. Above Mach 1, the entire flow field reorganizes around oblique shocks and expansion fans, requiring supersonic aerodynamic theory.

Sources & Methodology

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Frequently Asked Questions

  • The speed of sound depends on air temperature, not altitude or pressure directly. Because temperature decreases with altitude in the troposphere (−6.5°C/km), the speed of sound decreases. In the stratosphere, temperature stabilizes, and so does the speed of sound.