Gaussian Beams and 3-D Bottom Interacting Acoustic Systems
The analysis of the performance of current array systems requires accurate propagation modeling. In addition, future signal processing algorithms may incorporate a propagation model in order to obtain improved target tracking. The acoustic field received at an array of sensors located on or near the ocean bottom is strongly affected by the local bathymetry and by the physical properties of the ocean subbottom. At very low frequencies, the acoustic field may even be affected by the physical properties of the basement underlying the top sediment layers. This paper describes two techniques based on Gaussian beam tracing for computing the acoustic field in such an environment. The first method employs empirically derived formulas governing the spread of the beams and has the advantage of great simplicity. In the second method the beam curvature and width are obtained formally from an ordinary differential equation along the central ray. This latter method has recently received a lot of attention in the seismological community. Both methods are free of the difficulties at caustics and in shadow zones which afflict standard ray tracing algorithms. Comparisons are presented between the standard ray tracing, simplified beam tracing, formal beam tracing and the exact solution for a difficult negative sound speed gradient problem previously examined by Pedersen and Gordon. Finally, a detection system is proposed that employs Gaussian beam tracing convolved with target tracking.
KeywordsGaussian Beam Acoustic Field Ocean Bottom Stoneley Wave Shadow Zone
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- 1.J. L. Worzel and M. Ewing, Explosion sounds in shallow water, Section I, pp. 1–53 in Geological Society of America, Memoir 27, (1948).Google Scholar
- 2.C. L. Pekeris, Theory of propagation of explosive sound in shallow water, Sect. II, pp. 1–117 in Geological Society of America, Memoir 27 (1948).Google Scholar
- 6.E. L. Hamilton, R. T. Bachman, R. T. Berger, W. R. Johnson and L. A. Mayer, “Acoustic and related properties of calcareous deep-sea sediments,” J. Sedimentary Petrology, No. 52, pp. 733–753 (1982).Google Scholar
- 7.O. F. Hastrup, “Some bottom-reflection loss anomalies near grazing and their affect on propagation in shallow water,” pp. 135–152 in Ref. 18.Google Scholar
- 8.T. Akal, “Sea floor affects on shallow-water acoustic propagation,” pp. 557–575 in Ref. 18.Google Scholar
- 16.F. D. Tappert, “The parabolic equation method,” Sect. V in Lecture Notes in Physicis, No. 70, Ed. by J. B. Keller and J. S. Papadakis, Springer Verlag, Berlin, 1977.Google Scholar
- 17.Physics of Sound in Marine Sediments, ed, by Loyd Hampton, Plenum Press, New York, 1974.Google Scholar
- 18.Bottom Interacting Acoustics, ed. by W. Kuperman and F. Jensen, Plenum Press, New York, 1980.Google Scholar
- 22.H. P. Bucker, “Some comments on ray theory with examples from current NUC ray trace models,” pp. 32–36 in SACLANT Conf. Proceed., No. 5, (1971).Google Scholar