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Volumn 124, Issue 1, 2008, Pages 113-127

Temporal coherence of sound transmissions in deep water revisited

Author keywords

[No Author keywords available]

Indexed keywords

ACOUSTIC WAVE PROPAGATION; ACOUSTICS; ARCHITECTURAL ACOUSTICS; BATHYMETRY; INTEGRAL EQUATIONS; PROGRAMMABLE LOGIC CONTROLLERS; QUANTUM THEORY;

EID: 47649093382     PISSN: 00014966     EISSN: None     Source Type: Journal    
DOI: 10.1121/1.2932337     Document Type: Article
Times cited : (28)

References (37)
  • 3
    • 0032783811 scopus 로고    scopus 로고
    • Most work on matched field processing assumed a stationary ocean. The importance of temporal coherence for matched field localization was addressed in, "," J. Acoust. Soc. Am..
    • Most work on matched field processing assumed a stationary ocean. The importance of temporal coherence for matched field localization was addressed in K. Yoo and T. C. Yang, " Broadband source localization in shallow water in the presence of internal waves.," J. Acoust. Soc. Am. 106, 3255-3269 (1999).
    • (1999) Broadband Source Localization in Shallow Water in the Presence of Internal Waves , vol.106 , pp. 3255-3269
    • Yoo, K.1    Yang, T.C.2
  • 23
    • 47649124893 scopus 로고    scopus 로고
    • Proceedings of the Eighth European Conference on Underwater Acoustics, edited by S. M. Jesus and O. C. Rodrigues
    • T. C. Yang, " Comparison of temporal coherence of signal propagation in shallow and deep water.," Proceedings of the Eighth European Conference on Underwater Acoustics, edited by, S. M. Jesus, and, O. C. Rodrigues, 2006, pp. 169-174.
    • (2006) Comparison of Temporal Coherence of Signal Propagation in Shallow and Deep Water , pp. 169-174
    • Yang, T.C.1
  • 26
    • 0343858310 scopus 로고    scopus 로고
    • Littoral coherence limitations on acoustic arrays," in, edited by S. Lees and L. A. Ferrari (Plenum, New York), Vol. and references therein.
    • K. D. Rolt and P. A. Abbot, " Littoral coherence limitations on acoustic arrays.," in Acoustic Imaging, edited by, S. Lees, and, L. A. Ferrari, (Plenum, New York, 1997), Vol. 23 and references therein.
    • (1997) Acoustic Imaging , vol.23
    • Rolt, K.D.1    Abbot, P.A.2
  • 32
    • 47649087229 scopus 로고    scopus 로고
    • Proceedings of the Internal Conference on Underwater Acoustic Measurements: Technologies and Results, edited by J. S. Papadakis and L. Bjorno Heraklion, Greece, June.
    • J. Sellschopp, " High resolution measurements of the ocean fine structure and their relation to sound transmission.," Proceedings of the Internal Conference on Underwater Acoustic Measurements: Technologies and Results, edited by, J. S. Papadakis, and, L. Bjorno, Heraklion, Greece, June 2005.
    • (2005) High Resolution Measurements of the Ocean Fine Structure and Their Relation to Sound Transmission
    • Sellschopp, J.1
  • 34
    • 47649132476 scopus 로고    scopus 로고
    • Proceedings of the Fifth European Conference on Underwater Acoustics, edited by M. E. Zakharia, P. Chervet and P. Dubail, Lyon, France, 11-14 July
    • T. C. Yang and M. Siderius, " Temporal coherence and fluctuation of acoustic signals in shallow water.," Proceedings of the Fifth European Conference on Underwater Acoustics, edited by, M. E. Zakharia, P. Chervet, and, P. Dubail, Lyon, France, 11-14 July 2000, pp. 63-68.
    • (2000) Temporal Coherence and Fluctuation of Acoustic Signals in Shallow Water , pp. 63-68
    • Yang, T.C.1    Siderius, M.2
  • 37
    • 0015371215 scopus 로고
    • A geometric ray has a phase kz z, where z is the depth of the ray. The WKB approximation of a normal mode depth function has a phase ± ∞ z′ z kz (z, km) dz for upward and downward traveling waves where kz = k2 (z) - km2; z′ is a constant. See, for example, "," J. Acoust. Soc. Am.,. Hence for the path integral, ei kz z is replaced by the mode depth function, and for the second moment, one inserts the mode depth-function squared, integrated over depth.
    • A geometric ray has a phase kz z, where z is the depth of the ray. The WKB approximation of a normal mode depth function has a phase ± ∞ z′ z kz (z, km) dz for upward and downward traveling waves where kz = k2 (z) - km2; z′ is a constant. See, for example, L. Tolstoy, " The W.K.W. Approximation, turning points and the measurement of phase velocities.," J. Acoust. Soc. Am. 52, 356-363 (1972). Hence for the path integral, ei kz z is replaced by the mode depth function, and for the second moment, one inserts the mode depth-function squared, integrated over depth.
    • (1972) The W.K.W. Approximation, Turning Points and the Measurement of Phase Velocities , vol.52 , pp. 356-363
    • Tolstoy, L.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.