The intensity coherence function of time for partially saturated acoustic propagation through internal waves is calculated with a method that is improved over previous treatments. Two specific improvements are introduced: the usual expansion in is carried out to a higher order, and then the terms of that expansion are calculated with a new perturbative method. The method is applied to propagation without a sound channel, for both phase-screen and continuous-medium cases. The validity of the new perturbative method is estimated by calculating the next order error terms. Accuracies at the few-percent level are found. The new analytic formulas are also corroborated with numerical integration. Finally, the method is applied to a specific ocean-acoustic experiment [Azores Fixed Acoustic Range (AFAR)]. In order to achieve good agreement with experiment it will be necessary to add an accurate treatment of the sound channel to the present perturbation method.
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February 2001
February 01 2001
The intensity coherence function of time for partially saturated acoustic propagation through ocean internal waves
James S. Gerber;
James S. Gerber
Physics Department and Institute of Tectonics, University of California at Santa Cruz, Santa Cruz, California 95064
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Stanley M. Flatté
Stanley M. Flatté
Physics Department and Institute of Tectonics, University of California at Santa Cruz, Santa Cruz, California 95064
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J. Acoust. Soc. Am. 109, 528–537 (2001)
Article history
Received:
August 05 1999
Accepted:
September 06 2000
Citation
James S. Gerber, Stanley M. Flatté; The intensity coherence function of time for partially saturated acoustic propagation through ocean internal waves. J. Acoust. Soc. Am. 1 February 2001; 109 (2): 528–537. https://doi.org/10.1121/1.1322020
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