2020
DOI: 10.1121/10.0001627
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Passive broadband source depth estimation in the deep ocean using a single vector sensor

Abstract: For an acoustic receiver deployed at the bottom of the direct arrival zone of a submerged source at short horizontal ranges in deep ocean, the interference pattern of the direct and surface-reflected acoustic arrivals shows periodic modulation, which is directly related to the source depth, source frequency, and vertical arrival angle. In this work, the interference cycle presented in the frequency domain is used to extract the broadband source depth, with the vertical arrival angle obtained from the ratio of … Show more

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Cited by 17 publications
(3 citation statements)
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“…Therefore, they have become increasingly popular in deep-sea environments in recent years. Qi et al [22] and Li et al [23] employed a single vector hydrophone positioned near the seafloor to obtain the arrival angle and then estimated source depth based on the interference period of the received sound intensity spectrum. According to the estimated depth, Li further performed range estimation.…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, they have become increasingly popular in deep-sea environments in recent years. Qi et al [22] and Li et al [23] employed a single vector hydrophone positioned near the seafloor to obtain the arrival angle and then estimated source depth based on the interference period of the received sound intensity spectrum. According to the estimated depth, Li further performed range estimation.…”
Section: Introductionmentioning
confidence: 99%
“…Cao et al [16] applied a convolutional neural network to vector data and proposed a method of DOA estimation using an SVS based on deep transfer learning. Qi et al [17] used the interference cycle in the frequency domain to extract the source depth from signals recorded by an ocean-bottom seismometer (OBS) at a low frequency from 20 to 100 Hz.…”
Section: Introductionmentioning
confidence: 99%
“…Qi et al. [17] used the interference cycle in the frequency domain to extract the source depth from signals recorded by an ocean‐bottom seismometer (OBS) at a low frequency from 20 to 100 Hz.…”
Section: Introductionmentioning
confidence: 99%