Two sets of equations, covering all world oceans and seas, are presented to calculate pressure from depth for the computation of sound speed, and depth from pressure for use in ocean engineering. They are based on the algorithm of UNESCO 1983 [N. P. Fofonoff and R. C. Millard, Jr., Unesco Tech. Papers in Mar. Sci. No. 44 (1983)], and on calculations from temperature and salinity profiles. The pressure to depth conversion is presented first. The equations can be used in those cases where the desired accuracy is reduced to ±0.8 m. The equations to convert depth to pressure provide an overall accuracy between ±8000 Pa and ±1000 Pa. This leads to errors in sound speed consistently smaller than ±0.02 m/s. The discussion, and comparisons with results and other formulas, suggest that the new equations are a substantial improvement on the previous simplified ones, which should now be abandoned.
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March 1998
March 01 1998
Depth-pressure relationships in the oceans and seas
Claude C. Leroy;
Claude C. Leroy
Private consultant, Cabinet d’Etudes en Acoustique Sous-Marine, 41 rue du Docteur Clément, 83330 Le Plan du Castellet, France
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François Parthiot
François Parthiot
Chief of Department of Underwater systems at GENAVIR, IFREMER, B.P. 330, 83507 La Seyne-sur-Mer Cedex, France
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J. Acoust. Soc. Am. 103, 1346–1352 (1998)
Article history
Received:
March 28 1997
Accepted:
November 21 1997
Connected Content
A correction has been published:
Erratum: “Depth-pressure relationships in the oceans and seas” [J. Acoust. Soc. Am. 103(3), 1346–1352 (1998)]
Citation
Claude C. Leroy, François Parthiot; Depth-pressure relationships in the oceans and seas. J. Acoust. Soc. Am. 1 March 1998; 103 (3): 1346–1352. https://doi.org/10.1121/1.421275
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