Observations of phase and intensity fluctuations for low-frequency, long-range transmissions in the Philippine Sea and comparisons to path-integral theory

In the Philippine Sea, from April 2010 to March 2011, a 330-km radius pentagonal acoustic transceiver array with a sixth transceiver in the center transmitted broadband signals with center frequencies between 172 and 275 Hz and 100 Hz bandwidth eight times a day every other day. The signals were rec...

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Bibliographic Details
Main Authors: Chandrayadula, T.K (Author), Colosi, J.A (Author), Cornuelle, B.D (Author), Dzieciuch, M.A (Author), Worcester, P.F (Author)
Format: Article
Language:English
Published: Acoustical Society of America 2019
Subjects:
Online Access:View Fulltext in Publisher
LEADER 02766nam a2200421Ia 4500
001 10.1121-1.5118252
008 220511s2019 CNT 000 0 und d
020 |a 00014966 (ISSN) 
245 1 0 |a Observations of phase and intensity fluctuations for low-frequency, long-range transmissions in the Philippine Sea and comparisons to path-integral theory 
260 0 |b Acoustical Society of America  |c 2019 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1121/1.5118252 
520 3 |a In the Philippine Sea, from April 2010 to March 2011, a 330-km radius pentagonal acoustic transceiver array with a sixth transceiver in the center transmitted broadband signals with center frequencies between 172 and 275 Hz and 100 Hz bandwidth eight times a day every other day. The signals were recorded on a large-aperture vertical-line array located near the center of the pentagon at ranges of 129, 210, 224, 379, 396, and 450 km. The acoustic arrival structures are interpretable in terms of ray paths. Depth and time variability of the acoustic observations are analyzed for six ray paths (one from each transceiver) with similar vertical sampling properties in the main thermocline. Acoustic-field statistics treated include: (1) variances of phase and intensity, (2) vertical coherence and intensity covariance, (3) glinting and fadeout rates, and (4) intensity probability density functions. Several observed statistics are compared to predictions using Feynman path-integral theory assuming the Garrett-Munk internal-wave spectrum. In situ oceanographic observations support this assumption and are used to estimate spectral parameters. Data and theory differ at most by a factor of two and reveal the wave propagation regimes of unsaturated, partially saturated, and fully saturated. Improvements to the evaluation of path-integral quantities are discussed. © 2019 U.S. Government. 
650 0 4 |a Acoustic fields 
650 0 4 |a article 
650 0 4 |a covariance 
650 0 4 |a Feynman path integrals 
650 0 4 |a Intensity fluctuations 
650 0 4 |a Partially saturated 
650 0 4 |a Path-integral theory 
650 0 4 |a prediction 
650 0 4 |a probability 
650 0 4 |a Probability density function 
650 0 4 |a Propagation regimes 
650 0 4 |a Quantum theory 
650 0 4 |a sampling 
650 0 4 |a Spectral parameters 
650 0 4 |a statistics 
650 0 4 |a thermocline 
650 0 4 |a Transceivers 
650 0 4 |a Vertical coherence 
650 0 4 |a Vertical line arrays 
650 0 4 |a Wave propagation 
700 1 |a Chandrayadula, T.K.  |e author 
700 1 |a Colosi, J.A.  |e author 
700 1 |a Cornuelle, B.D.  |e author 
700 1 |a Dzieciuch, M.A.  |e author 
700 1 |a Worcester, P.F.  |e author 
773 |t Journal of the Acoustical Society of America