2022
DOI: 10.1134/s0015462822010062
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Modeling of Unsteady Geophysical Processes on the Shelf of the Sea of Japan

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Cited by 9 publications
(1 citation statement)
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“…For example, to study background fluctuations in the sound speed, when amplitudes of these fluctuations are 1-2 m/s, it is required to measure salinity with an accuracy of 0.1-0.2 psu, because @c/@s ≈ 1 [m/s]/psu (Figure 14). Increased requirements for the accuracy of determining the density of water may also arise for calculating the equations of multilayer shallow water [54]. The range of salinity variation in the study area of Peter the Great Bay (the Sea of Japan) is about 3 psu, which is why using some average salinity for solving the set tasks is unacceptable.…”
Section: Discussionmentioning
confidence: 99%
“…For example, to study background fluctuations in the sound speed, when amplitudes of these fluctuations are 1-2 m/s, it is required to measure salinity with an accuracy of 0.1-0.2 psu, because @c/@s ≈ 1 [m/s]/psu (Figure 14). Increased requirements for the accuracy of determining the density of water may also arise for calculating the equations of multilayer shallow water [54]. The range of salinity variation in the study area of Peter the Great Bay (the Sea of Japan) is about 3 psu, which is why using some average salinity for solving the set tasks is unacceptable.…”
Section: Discussionmentioning
confidence: 99%