Sound Speed in Water Calculator

Sound travels about 1,482 m/s in fresh water at 20 °C and about 1,507 m/s in seawater at 15 °C and 35 ppt. Speed rises about 2–4.6 m/s per °C (most in cold water), 1.3 m/s per ppt of salinity and 1.6–1.7 m/s per 100 m of depth.

Use the Sound Speed in Water Calculator

Water & Equation

Each equation is used only inside its published range.

Temperature Scale
Depth Scale
2.0 to 30.0 °C
25.0 to 40.0 ppt

Open ocean ≈ 35 ppt; Baltic ≈ 7; brackish estuaries 0.5–30 (use UNESCO or Coppens below 25).

0 to 8,000 m
Presets
Calculated Sound Speed Mackenzie (1981)
SI Velocity (m/s)
—
Feet / second—
Miles / hour (mph)—
Kilometres / hour—
Knots (nmi/h)—
Equation comparison m/s
Term Breakdown m/s
Echo range & wavelength
Range / depth—
Wavelength—
Equation used & validity

Sources: UK NPL seawater equations (UNESCO, Mackenzie, Coppens, Leroy & Parthiot), Lubbers & Graaff (1998), Marczak (1997) J. Acoust. Soc. Am. 102, 2776, and NIST SP 811.

Speed of sound in water by temperature (surface pressure)

Fresh water: Marczak (1997). Seawater 35 ppt: UNESCO / Wong & Zhu (1995), valid to 40 °C.

Temp Fresh m/s Fresh ft/s Seawater m/s Seawater ft/s
0 °C (32 °F) 1,402.4 4,601 1,449.1 4,754
4 °C (39 °F) 1,421.6 4,664 1,466.6 4,812
5 °C (41 °F) 1,426.2 4,679 1,470.7 4,825
10 °C (50 °F) 1,447.3 4,748 1,489.8 4,888
15 °C (59 °F) 1,466.0 4,810 1,506.7 4,943
20 °C (68 °F) 1,482.4 4,863 1,521.5 4,992
25 °C (77 °F) 1,496.7 4,911 1,534.4 5,034
30 °C (86 °F) 1,509.2 4,951 1,545.6 5,071
35 °C (95 °F) 1,519.8 4,986 1,555.2 5,102
40 °C (104 °F) 1,528.9 5,016 1,563.2 5,129
50 °C (122 °F) 1,542.6 5,061 — —
60 °C (140 °F) 1,551.0 5,089 — —
74 °C (165 °F) 1,555.1 5,102 — —
80 °C (176 °F) 1,554.5 5,100 — —
90 °C (194 °F) 1,550.5 5,087 — —

Worked examples

Ocean surface. T = 15 °C, S = 35 ppt, D = 0: UNESCO 1,506.68 m/s, Mackenzie 1,506.69 m/s, Coppens 1,506.65 m/s.

1,000 m deep, 4 °C. Pressure at 45° latitude is 100.9 bar (Leroy & Parthiot). UNESCO gives 1,483.23 m/s, Mackenzie 1,482.96 m/s and Coppens 1,483.02 m/s; about 23 m/s slower than the surface despite the higher pressure, because the water is 11 °C colder.

Fresh water. 20 °C: Marczak 1,482.38 m/s, Lubbers & Graaff 1,482.30 m/s. A 40 ms echo at 1,482.4 m/s is 29.65 m away.

Copied to clipboard

Summary

The speed of sound in water depends on temperature, salinity and pressure (depth). This calculator offers the standard published equations and labels which one produced each result: for seawater the UNESCO algorithm of Chen and Millero as refitted by Wong and Zhu (1995) for ITS-90, the nine-term Mackenzie (1981) equation and the Coppens (1981) equation; for fresh water the Marczak (1997) fit valid from 0 to 95 °C and the Lubbers & Graaff (1998) equation for 15–35 °C. Depth is converted to pressure for the UNESCO equation with the Leroy and Parthiot (1998) formula at your latitude. A comparison table shows every equation side by side, and the result feeds an echo-sounder range and wavelength helper.

How it works

  1. Pick seawater or fresh water, then the equation. Each equation is only evaluated inside its published validity range.
  2. Enter temperature (°C or °F), and for seawater salinity (ppt or PSU), depth (m or ft) and, for UNESCO, latitude.
  3. UNESCO: c = Cw(T,P) + A(T,P)·S + B(T,P)·S^1.5 + D(T,P)·S², with pressure in bar from depth by Leroy & Parthiot (1998).
  4. Mackenzie (1981): c = 1448.96 + 4.591T − 0.05304T² + 0.0002374T³ + 1.340(S − 35) + 0.0163D + 1.675×10⁻⁷D² − 0.01025T(S − 35) − 7.139×10⁻¹³TD³.
  5. Fresh water, Marczak (1997): c = 1402.385 + 5.038813T − 5.799136×10⁻²T² + 3.287156×10⁻⁴T³ − 1.398845×10⁻⁶T⁴ + 2.787860×10⁻⁹T⁵.
  6. Range from an echo: distance = c × two-way travel time ÷ 2. Wavelength = c ÷ frequency.

Use cases

  • Set the sound velocity for an echo sounder, sonar, ADCP or acoustic modem from a temperature and salinity reading.
  • Convert two-way travel time to depth or range.
  • Find the speed of sound in fresh water for ultrasonic flow meters, tank level sensors and lab transducers, including hot water up to 95 °C.
  • Compare UNESCO, Mackenzie and Coppens results to see the spread between standard equations.
  • Teach how temperature, salinity and pressure each change underwater sound speed.

Frequently Asked Questions

Last updated: 2026-10-10 · Reviewed by Nham Vu