Estimation of the spatial variability of the New England Mud Patch geoacoustic properties using a distributed array of hydrophones and deep learninga)
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Summary
This summary is machine-generated.Deep learning rapidly models seafloor sediment properties using impulse signals. This efficient method reveals spatial variations in sound speed, aiding underwater acoustic studies.
Area Of Science
- Oceanography
- Geophysics
- Acoustics
Background
- Geoacoustic inversion traditionally demands substantial computational power.
- Understanding shallow water sediment properties is crucial for acoustic modeling.
- Previous methods lacked efficiency for large-scale spatial analysis.
Purpose Of The Study
- To develop and validate a deep learning (DL) based spatial environmental inversion scheme.
- To model a single spatially-varying sediment layer using broadband impulse signals.
- To analyze sediment sound speed and sound speed ratio in the New England Mud-Patch (NEMP).
Main Methods
- Utilized deep learning (DL) with broadband impulse signals for inversion.
- Applied the scheme to synthetic data simulating Seabed Characterization Experiment 2022 (SBCEX22) conditions.
- Processed 1836 signals from bottom-moored hydrophones using a neural network for rapid inversion.
Main Results
- Successfully predicted the lateral spatial structure of sediment sound speed and its ratio with water sound speed.
- Validated the DL inversion scheme on a range-dependent synthetic test set.
- Observed a southwest to northeast increase in compressional sound speed and sound speed ratio in the NEMP.
Conclusions
- Deep learning offers an efficient alternative to traditional geoacoustic inversion methods.
- The DL approach enables rapid processing of numerous signals for spatial analysis.
- The findings are consistent with existing geological and acoustic data from the NEMP, highlighting DL's potential in shallow water geoacoustic inversion.

