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Several merchant ship-radiated noise events were recorded in two separate seabed characterization experiments in the New England Mudpatch region in 2017 (SBCEX17) and 2022 (SBCEX22). These shallow water acoustic experiments were conducted under different oceanographic conditions, resulting in fluctuations in sound propagation. Several statistical inference approaches are used to invert geo-acoustic parameters such as sound speed and density in a mud over sand sediment (See https://doi.org/10.1121/10.0008419). In this work, we explore the effect of sound speed profile fluctuations in the water column on geo-acoustic inversions in the 360–1100 Hz frequency band. Inversions based on measured and simulated data using acoustic models are provided to support our findings. The results demonstrate that sediment parameters become more sensitive to oceanographic variations as the frequency increases and, therefore, sound speed profile fluctuations in the water column need to be taken into close consideration for more accurate geo-acoustic inversions. Work supported by ONR.
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Escobar-Amado et al. (Fri,) studied this question.
synapsesocial.com/papers/68e76bd8b6db6435876e1e7d — DOI: https://doi.org/10.1121/10.0026913
Christian D. Escobar-Amado
University of Delaware
Mohsen Badiey
University of Delaware
The Journal of the Acoustical Society of America
University of Delaware
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