Speed of Sound Calculator
Calculate the speed of sound in air, water, steel, wood, and other materials. This acoustic velocity calculator adjusts for temperature, returns wavelengths for any frequency, and compares media side-by-side.
Medium & Temperature
Results
Speed of Sound in Common Materials
| Medium | Speed (m/s) | Speed (ft/s) | Relative to Air | Notes |
|---|---|---|---|---|
| Air (20°C) | 343 | 1125 | 1× | Temperature-dependent |
| Air (0°C) | 331 | 1086 | 0.97× | Reference condition |
| Helium (20°C) | 965 | 3166 | 2.81× | High γ/M ratio |
| Hydrogen (20°C) | 1270 | 4167 | 3.70× | Lowest molecular mass |
| Fresh Water (20°C) | 1481 | 4859 | 4.32× | Temperature + pressure sensitive |
| Sea Water (20°C) | 1522 | 4993 | 4.43× | Salinity raises speed |
| Concrete | 3100 | 10170 | 9.0× | Varies by mix |
| Wood (oak) | 3850 | 12631 | 11.2× | Along grain |
| Glass | 5640 | 18504 | 16.4× | Compressive wave |
| Aluminum | 6320 | 20735 | 18.4× | Longitudinal wave |
| Steel | 5960 | 19554 | 17.4× | Longitudinal wave |
How to Use the Speed of Sound Calculator
- Select a medium — choose from air, water, metals, or other materials.
- Set temperature — for gases, temperature significantly changes sound speed. Use the slider or type a value. Switch between °C, °F, or K.
- Enter frequency — the tool shows the corresponding wavelength at that frequency in the selected medium.
- Read results — speed appears in m/s, km/h, mph, ft/s, and as a Mach number relative to standard air.
- Copy results — click Copy Result to copy the full summary to your clipboard.
Speed of Sound Formulas Explained
Why Does Temperature Affect Sound Speed?
Sound travels by transferring kinetic energy between molecules through collisions. At higher temperatures, gas molecules move faster and collide more frequently, transmitting energy more quickly. This is why sound travels faster on a hot day. The acoustic velocity of a gas is therefore a direct function of its thermodynamic temperature, not its pressure — at constant temperature, doubling the pressure leaves sound speed unchanged because both density and bulk modulus rise equally.
The exact relationship: every 1°C increase raises air sound speed by approximately 0.6 m/s. The standard sound speed formula for dry air is v = 331.4 + 0.6 × T(°C), accurate to within 0.1 m/s across the range −30°C to +50°C. At 0°C, sound travels at 331.4 m/s. At 20°C (room temperature), it travels at 343.4 m/s. At 40°C it reaches 355.4 m/s. Humidity has a small but real effect: moist air is slightly less dense than dry air (water vapour is lighter than diatomic nitrogen and oxygen), raising the speed by roughly 0.3–0.5 m/s at 50% relative humidity.
In liquids and solids, the temperature dependence is more complex — water actually slows down above 74°C due to structural changes, while metals typically slow as they expand with heat. The acoustic impedance of a medium (Z = ρ × v, in Pa·s/m or rayl) also changes with temperature, which matters for reflection and transmission calculations at boundaries.
Practical Applications
- Sonar & Underwater Acoustics — submarines and fish finders must account for temperature, salinity, and depth gradients that change sound speed by 10–15%. The ocean's SOFAR channel (Sound Fixing and Ranging) is a minimum-speed layer at around 700–1200 m depth where sound becomes trapped and can propagate thousands of kilometres.
- Ultrasonic Testing (NDT) — defect detection in metals relies on knowing exact sound speed in the material to locate cracks by time-of-flight. For a quick reference wavelength at your test frequency, the wavelength calculator covers fluids, metals, and tissue.
- Echo Distance Measurement — distance = (v × time) / 2. Temperature corrections are critical for accurate ranging; an uncorrected 10°C error in air introduces about 0.9% distance error.
- Room Acoustics — speaker delay alignment in live sound requires knowing the speed so delay lines are set correctly (distance / speed = delay time). The Doppler effect calculator extends this to moving sources and receivers.
- Aviation — Mach number = aircraft speed / local speed of sound (which decreases with altitude as temperature drops). The speed of sound at altitude is lower than at sea level precisely because the ISA temperature lapse rate cools the air; at 11,000 m, temperature stabilises at −56.5°C and sound speed settles at ~295 m/s.