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Performance study of ray-based ocean acoustic tomography methods for estimating submesoscale variability in the upper
Etienne Ollivier1, Richard X Touret2, Matthew McKinley1
1Woodruff School of Mechanical Engineering, Georgia Institute of Technology, Atlanta, Georgia 30332, USA.
The Journal of the Acoustical Society of America
|February 13, 2024
Summary
Ocean acoustic tomography (OAT) effectively estimates upper ocean sound speed profiles (SSPs) using simulated data. This research optimizes OAT configurations and methods for monitoring submesoscale variability with autonomous platforms.
Area of Science:
- Oceanography
- Acoustics
- Geophysics
Background:
- Ocean acoustic tomography (OAT) estimates sound speed profiles (SSPs) using acoustic travel times.
- Understanding upper ocean dynamics requires accurate, high-resolution SSP data.
- Submesoscale variability significantly impacts ocean processes but is challenging to monitor.
Purpose of the Study:
- To investigate the estimation of range-dependent SSPs in the upper ocean using OAT.
- To evaluate OAT performance for monitoring submesoscale ocean variability.
- To provide practical guidance for designing future OAT experiments.
Main Methods:
- Simulated three-dimensional sound speed variations in the DeSoto Canyon using a regional ocean circulation model.
- Applied classical ray-based OAT and iterative/adaptive OAT formulations.
- Investigated OAT performance based on source-receiver configuration, OAT estimator, and inversion duration.
Main Results:
- OAT performance is sensitive to source-receiver geometry and ray coverage.
- Iterative/adaptive OAT formulations show potential for improved SSP estimation.
- The duration of OAT inversion impacts the accuracy of capturing submesoscale variability.
Conclusions:
- OAT is a viable method for estimating range-dependent SSPs and monitoring submesoscale ocean variability.
- Optimized source-receiver configurations and adaptive algorithms enhance OAT effectiveness.
- Moving autonomous platforms can be effectively utilized in future OAT experiments for upper ocean monitoring.

