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Arrival-time structure of the time-averaged ambient noise cross-correlation function in an oceanic waveguide
Karim G Sabra1, Philippe Roux, W A Kuperman
1Marine Physical Laboratory, Scripps Institution of Oceanography, La Jolla, California 92103-0238, USA. ksabra@mpl.ucsd.edu
The Journal of the Acoustical Society of America
|February 12, 2005
Summary
Deterministic arrival times are extracted from ambient noise cross-correlations. This finding, observed in seismology and acoustics, aids in understanding wave propagation using noise data.
Area of Science:
- Acoustics
- Seismology
- Wave Propagation
Background:
- Ambient noise cross-correlation is a technique used to infer Earth's structure.
- Experimental observations have confirmed coherent arrival times in various environments.
- Existing formulations of ambient noise cross-correlation lack detailed source distribution analysis.
Purpose of the Study:
- To demonstrate a method for extracting coherent deterministic arrival times from ambient noise.
- To analyze the influence of noise source distribution and receiver bandwidth on arrival times.
- To compare derived formulations with existing methods for ambient noise cross-correlation.
Main Methods:
- Utilizing a time-domain image formulation of the noise cross-correlation function.
- Analyzing a uniform distribution of noise sources within a Pekeris waveguide.
- Investigating the derivative of the time-averaged ambient noise cross-correlation function.
Main Results:
- Coherent deterministic arrival times can be extracted from the derivative of the noise cross-correlation function.
- The image formulation reveals the impact of noise source distribution (range and depth) on arrival times.
- Receiver bandwidth significantly influences the arrival-time structure.
Conclusions:
- The study provides a clear demonstration of extracting deterministic arrival times from ambient noise.
- The developed image formulation offers a practical tool for analyzing noise cross-correlation data.
- Findings have direct implications for interpreting data from oceanographic and seismic experiments.