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Speed of Sound Calculator

Result

343.42m/s

Result: 343.42 m/s

Sound travels through dry air at 331.3 m/s at freezing point and gains about 0.606 m/s for every degree Celsius: 343.42 m/s at 20 °C. Warmer air means faster molecules and a quicker relay. Humidity and altitude shift the figure slightly, so treat it as a close everyday approximation.

The numbers at a glance

Air temperature (°C) (°C)Result (m/s)
0.00331.30
5.00334.33
10.00337.36
15.00340.39
20.00Your value343.42
25.00346.45
30.00349.48
35.00352.51
40.00355.54

Worked examples

How it's calculated

v = 331.3 + 0.606 × T

  1. StepEnter the air temperature in degrees Celsius.
  2. StepEvery degree adds about 0.606 m/s to the 331.3 m/s baseline.
  3. ResultRead the speed in metres per second — divide a distance by it to get the delay.

Reference table

Air temperature (°C)SettingSpeed of sound (m/s)
-40Cruising altitude of an airliner307.06
0Freezing point of water331.3
20Room temperature343.42
25Warm summer day346.45
100Boiling point of water391.9

Questions

How do I calculate the speed of sound in air?

Use the dry-air approximation v = 331.3 + 0.606 × T, where T is the air temperature in °C and v comes out in metres per second. At 20 °C that gives 331.3 + 0.606 × 20 = 343.42 m/s. Add about 0.6 m/s for every degree the air warms up.

Why does temperature change the speed of sound?

Sound travels by molecules bumping into their neighbours. Warmer air has faster-moving molecules, so the disturbance passes along more quickly. Each extra degree Celsius adds roughly 0.6 m/s, which is why sound is about 331 m/s at 0 °C but around 343 m/s at 20 °C.

What is the speed of sound at 0 °C?

At 0 °C the formula gives 331.3 + 0.606 × 0 = 331.3 m/s. This is the intercept of the linear approximation — the speed of sound in dry air at the freezing point of water. Reference works quote values between 331.3 and 331.6 m/s, so the last decimal is not settled.

Do humidity and altitude affect the result?

Slightly — this formula assumes dry air, but humid air is a little less dense and carries sound marginally faster, usually well under 1 percent. Altitude changes the speed mainly through temperature, not pressure directly. For everyday use the dry-air figure is a close approximation.

What can I use the speed of sound for?

Estimating distances from echoes and thunder is the classic use: sound covers about 343 m every second at 20 °C, so a thunderclap heard 3 seconds after the lightning is roughly 1 km away. It also matters for music, acoustics, and timing sonar or ultrasonic sensors.

Sources and last check

  1. en.wikipedia.org

Information, not professional advice.