1981
DOI: 10.1121/1.385486
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Simple equations for the speed of sound in Neptunian waters

Abstract: Two simple equations for the speed of sound in sea waters, down to depths of 4 km, have been obtained as approximations to a more precise equation developed by Lovett. The simpler of the two is valid for all Neptunian waters except the Red Sea, Mediterranean Sea, and Persian Gulf, and agrees with Lovett’s equation to within about 0.1 m/s. The other includes these water masses and is in agreement with Lovett to within about 0.03 m/s. The two equations are well adapted to programmable handheld calculators.

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Cited by 90 publications
(43 citation statements)
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“…These results emphasize the importance of compensating for the influence of temperature and depth effect on the speed of sound during the trawl survey, assuming that both temperature and depth data are available. Similar results were obtained by Kotwicki et al (2011), who instead of Del Grosso (1974) used the formula of Coppens (1981) for the accurate estimate of the speed of sound. Their results have shown that after compensating for the temperature effect, the original measured swept area was overestimated for all tows.…”
Section: Discussionsupporting
confidence: 81%
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“…These results emphasize the importance of compensating for the influence of temperature and depth effect on the speed of sound during the trawl survey, assuming that both temperature and depth data are available. Similar results were obtained by Kotwicki et al (2011), who instead of Del Grosso (1974) used the formula of Coppens (1981) for the accurate estimate of the speed of sound. Their results have shown that after compensating for the temperature effect, the original measured swept area was overestimated for all tows.…”
Section: Discussionsupporting
confidence: 81%
“…However, the speed of sound in seawater is not constant because it depends on water temperature, pressure, and salinity (Chen and Millero 1977, Coppens 1981, Del Grosso 1974, Leroy et al 2008, Wong and Zhu 1995. Hall (2000), for example, noted that the speed of sound in water might change by approximately 3 m s -1 per 1°C.…”
Section: Introductionmentioning
confidence: 99%
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“…In Cheng et al (2009b), the authors combine USP and UPS to give rise to a multi-stage silent positioning system LSLS that (i) does not require time synchronization, (ii) only requires three surface buoys, (iii) incorporates smart anchor selection, and (iv) considers sound speed variation with temperature, salinity and depth using the model of Coppens (Coppens, 1981).…”
Section: Projection-based Localizationmentioning
confidence: 99%
“…Sound speeds in freshwater are slightly lower than those for seawater at the same temperature and depth. Empirical formulas for A-1 sound speeds in water as functions of temperature, depth, and salinity may be found in Coppens (1981).…”
Section: A12 Sound Speedmentioning
confidence: 99%