Abstract
Experimental data obtained by studying the sound field produced in the first and second convergence zones by an omnidirectional pseudonoise source operating in the kilohertz frequency range at a depth of ∼10 m are presented. The measurements of the cross correlation and the time spectra are performed for the signals received from different directions in the vertical plane by one narrow-beam, 40-m array and by two such arrays with the array centers positioned at different depths (200 and 450 m). The results of the experiments show that, for the signals arriving over different ray paths, the cross-correlation coefficients and the fluctuations of the time spectra obtained by using the reception at one depth and at two different depths are practically identical.
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Translated from Akusticheski\(\overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\smile}$}}{l}\) Zhurnal, Vol. 48, No. 1, 2002, pp. 44–51.
Original Russian Text Copyright © 2002 by Galkin, Pankova.
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Galkin, O.P., Pankova, S.D. Correlation structure of the sound field produced in a deep ocean by a near-surface sound source. Acoust. Phys. 48, 39–45 (2002). https://doi.org/10.1134/1.1435387
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DOI: https://doi.org/10.1134/1.1435387