c = 331.3 + 0.606·T
Speed of sound in air increases approximately linearly with temperature, since warmer air has a higher mean molecular speed.
Speed of sound in air increases approximately linearly with temperature, since warmer air has a higher mean molecular speed.
Select a target and calculate.
Speed of sound in air increases approximately linearly with temperature, since warmer air has a higher mean molecular speed.
T=20 °C gives c=331.3+0.606·20≈343.4 m/s.
Dry, still air at standard pressure; humidity, wind speed and temperature ranges far from 0 °C outside the linear approximation's valid range are excluded.
This calculator determines the speed of sound in dry air from air temperature, the basis for travel-time measurements such as echo sounding or ultrasonic sensing.
For dry air at standard pressure, the linear approximation c=331.3+0.606·T (T in °C) holds, derived from the more exact relation via the ideal gas law.
c = 331.3 + 0.606·T
c = 331.3 + 0.606·TT = (c−331.3)/0.606| Symbol / input | Meaning |
|---|---|
| Speed of sound c | Propagation speed of sound in still, dry air at the given temperature. |
| Air temperature T | Temperature of the air the sound propagates through. |
T is the air temperature through which the sound propagates.
Measure T at the location of sound propagation; use a representative average for larger temperature variation along the path.
T=20 °C gives c=331.3+0.606·20≈343.4 m/s.
Speed of sound rises with temperature; at a wintry −10 °C it falls to about 325 m/s, at a summery 30 °C it rises to about 349 m/s.
T is a temperature. c is output as a speed.
Basis for travel-time measurements (echo sounding, ultrasonic sensors, lightning-thunder distance estimation) and acoustic calculations generally.
Dry, still air at standard pressure; humidity (slightly raises c), wind speed, and temperatures far from 0 °C outside the linear approximation's valid range are excluded.
Common mistake: Do not confuse the speed of sound in vacuum or water with that in air; the values differ by more than a factor of four.
Basis for travel-time measurements (echo sounding, ultrasonic sensors, lightning-thunder distance estimation) and acoustic calculations generally.
T is the air temperature through which the sound propagates.
Dry, still air at standard pressure; humidity (slightly raises c), wind speed, and temperatures far from 0 °C outside the linear approximation's valid range are excluded.