2014
DOI: 10.1121/1.4871577
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Arrival-time fluctuations of coherent reflections from surface gravity water waves

Abstract: Arrival time fluctuations of coherent reflections from surface gravity waves are examined. A two-dimensional ray model with an evolving rough sea surface is used to explain the mechanism and formation of the deterministic striation patterns due to the surface reflection. Arrival time predictions from the ray model match qualitatively well with the measurements from bidirectional acoustic transmissions in a water depth of 100 m.

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Cited by 8 publications
(3 citation statements)
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“…Another design of upward-looking acoustic tools relies on sound scattering model to reconstruct surface spectrum moments basing on the Doppler spectrum of the reflected signal [12][13][14]. High frequency signals reverberation patterns may allow to track individual wave crests in vicinity of the transducer, as it has been reported by [15] and [16]. The mentioned tools are designed for local measurements and methods to assess waves and currents on a long range are of great interest too.…”
Section: Introductionmentioning
confidence: 99%
“…Another design of upward-looking acoustic tools relies on sound scattering model to reconstruct surface spectrum moments basing on the Doppler spectrum of the reflected signal [12][13][14]. High frequency signals reverberation patterns may allow to track individual wave crests in vicinity of the transducer, as it has been reported by [15] and [16]. The mentioned tools are designed for local measurements and methods to assess waves and currents on a long range are of great interest too.…”
Section: Introductionmentioning
confidence: 99%
“…The statistical distributions of received multipath fading signals in shallow water have been studied numerically and experimentally for underwater acoustic communication system design and performance analysis. [1][2][3][4][6][7][8][9][10][11][12][13][14][15] There is as yet no consensus on the fading statistics applicable in shallow water owing to various acoustical boundary conditions and applicable acoustic communication systems. However, representative statistics can be selected among these previous studies.…”
Section: Introductionmentioning
confidence: 99%
“…10 When the surface wave is smooth relative to source frequency, the interface of surface wave is considered to be partially flat and the pressure at the interface is computed using the reflection coefficient, 11 and the ray-based model can be applied as the previous works. [3][4][5][12][13][14][15] The benefit of the time-domain ray approach over the PE model is to enable tracking of the rays interacting with the surface wave causing the striation pattern. In our analysis, attenuation and scattering of sound by bubbles near the surface are not considered.…”
Section: Introductionmentioning
confidence: 99%