The speed of sound in the marine environment and its calculation (review)
UDC
534.231EDN
TTMCJGDOI:
10.31429/vestnik-23-3-55-67Abstract
For sound propagation in the seas and oceans, it is important to know not the absolute value of the speed of sound, but the shape of its profile. The range of sound propagation depends on the shape of the profile. The speed of sound propagation strongly depends on temperature (T, °C), salinity (S, ‰), and hydrostatic pressure (P, atm.). The article presents monthly average vertical profiles of temperature, sound velocity, and seasonal salinity profiles for the central part of the Black Sea. Temperature has the greatest effect on the speed of sound at sea. The axis of the underwater sound channel coincides with the minimum temperature value. The axis of the underwater sound channel is located at a depth of 35–55 m. In winter, the underwater sound channel is poorly expressed, practically absent. The axis of the underwater sound channel in the Black Sea, depending on the season, is located at a depth of 30–80 m. The paper presents the main empirical formulas for calculating the sound velocity profile in seawater. The analysis of empirical formulas is performed. Each of the above equations has its own error in calculating the speed of sound. The choice of an equation depends on the acceptable accuracy for its particular application.
Keywords:
sound propagation velocity, temperature, salinity, hydrostatic pressure, sea water, underwater sound channelFunding information
The study did not have sponsorship.
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