1970
DOI: 10.1121/1.1912133
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Statistics of Sound Propagation in the Ocean

Abstract: The statistics of transmission fluctuations in the ocean are examined theoretically for both multipath and scattering processes. It is shown that, when both are present, multipath propagation dominates the fluctuations and leads to quite broad statistical distributions. In such cases, the mean and standard deviation for logarithmic measures such as transmission loss differ considerably from corresponding mean-square measures. Results for a single tone have been generalized to include multitones, as a model of … Show more

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Cited by 96 publications
(62 citation statements)
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“…For example, at 1228 Hz the standard deviation when the source is on is on the order of 1 dB. When the source is off the standard deviation is on the order of 5 dB, in agreement with the 5.6 dB standard deviation of noise caused by distance sources predicted by Dyer [118]. Further, the peaks in the standard deviation seen for 220.5, 415, and 635 Hz correspond to the destructive interference nulls in the received signal levels where the received signal is noise dominated.…”
Section: Error Analysissupporting
confidence: 71%
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“…For example, at 1228 Hz the standard deviation when the source is on is on the order of 1 dB. When the source is off the standard deviation is on the order of 5 dB, in agreement with the 5.6 dB standard deviation of noise caused by distance sources predicted by Dyer [118]. Further, the peaks in the standard deviation seen for 220.5, 415, and 635 Hz correspond to the destructive interference nulls in the received signal levels where the received signal is noise dominated.…”
Section: Error Analysissupporting
confidence: 71%
“…2 )exp(y − exp(y)/2σ 2 ), the log density [118]. However, about the most probable point, the log density can be approximated by a gaussian density, which simplifies the analysis.…”
Section: Error Analysismentioning
confidence: 99%
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“…The resultant modal amplitudes for mode one incident are shown in [7] showed that for a fixed source and receiver in the SWARM95 experiment, situated across the mean direction of the internal wave crests, the root mean square of the log-intensity over a several hour time window was near 5.6 dB, the statistical value expected for fully saturated ocean waveguides [58,59]. …”
Section: A Multiple Wavesmentioning
confidence: 99%
“…He showed that for a fixed source and receiver situated across the mean direction of the internal wave crests, the root mean square of the log-intensity over a several hour time window was near 5.6 dB, the statistical value expected for fully saturated ocean waveguides. 37 …”
Section: B Multiple Wavesmentioning
confidence: 99%