2004•Unpublished venueRequires access

Vertical correlation of shallow-water reverberation and inversion for bottom reflection loss and bottom scattering strength

Guo Lianghao

Open publisher page 3 citations

Abstract

On the basis of the shallow-water normal mode combined with ray-mode analogies, the expression of reverberation vertical correlation is derived. Both of the theory and experiment data show: reverberation vertical correlation is independent on source depth, but dependent on receiver depth. A method of inversion for bottom reflection loss and bottom scattering strength is put forward. Reverberation intensity and vertical cross-correlation coefficients of reverberation are used in the inversion. The numerical and the experimental results show that the speed of inversion is fast and the inversion results are stable.

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What this paper is about

On the basis of the shallow-water normal mode combined with ray-mode analogies, the expression of reverberation vertical correlation is derived. Both of the theory and experiment data show: reverberation vertical correlation is independent on source depth, but dependent on receiver depth. A method of inversion for bottom reflection loss and bottom scattering strength is put forward. Reverberation intensity and vertical cross-correlation coefficients of reverberation are used in the inversion. The numerical and the experimental results show that the speed of inversion is fast and the inversion results are stable.

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Available abstract

On the basis of the shallow-water normal mode combined with ray-mode analogies, the expression of reverberation vertical correlation is derived. Both of the theory and experiment data show: reverberation vertical correlation is independent on source depth, but dependent on receiver depth. A method of inversion for bottom reflection loss and bottom scattering strength is put forward. Reverberation intensity and vertical cross-correlation coefficients of reverberation are used in the inversion. The numerical and the experimental results show that the speed of inversion is fast and the inversion results are stable.

Key concepts: Reverberation, Inversion (geology), Scattering, Waves and shallow water, Geology, Acoustics, Reflection (computer programming), Optics

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