Detection of Earthquake Infragravity and Tsunami Waves With Underwater Distributed Acoustic Sensing
Abstract
Underwater Distributed Acoustic Sensing (DAS) utilizes optical fiber as a continuous sensor array. It enables high-resolution data collection over long distances and holds promise to enhance tsunami early warning capabilities. This research focuses on detecting infragravity and tsunami waves associated with earthquakes and understanding their origin and dispersion characteristics through frequency-wavenumber domain transformations and beamforming techniques. We propose a velocity correction method based on adjusting the apparent channel spacing according to water depth to overcome the challenge of detecting long-wavelength and long-period tsunami signals. Experimental results demonstrate the successful retrieval of infragravity and tsunami waves using a subsea optical fiber in offshore Oregon. These findings underscore the potential of DAS technology to complement existing infragravity waves detection systems, enhance preparedness, and improve response efforts in coastal communities. Further research and development in this field are crucial to fully utilize the capabilities of DAS for enhanced tsunami monitoring and warning systems.
Copyright and License
© 2024. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited
Contributions
Conceptualization: Han Xiao
Data curation: Zack J. Spica
Formal analysis: Han Xiao
Funding acquisition: Zack J. Spica, Zhongwen Zhan
Investigation: Han Xiao, Zack J. Spica, Jiaxuan Li, Zhongwen Zhan
Methodology: Han Xiao, Zack J. Spica, Jiaxuan Li, Zhongwen Zhan
Project administration: Zhongwen Zhan
Resources: Han Xiao, Zack J. Spica, Jiaxuan Li, Zhongwen Zhan
Software: Han Xiao
Supervision: Zhongwen Zhan
Validation: Han Xiao
Visualization: Han Xiao
Writing – original draft: Han Xiao
Acknowledgement
The authors extend their gratitude to Editor Daoyuan Sun and the anonymous reviewers for their invaluable suggestions and inputs. The authors would like to thank Loïc Viens, Mohan Pan for their helpful suggestions. This work was supported by the Gordon Moore Foundation #9500 and National Science Foundation CAREER award 1848166. Z.J.S acknowledges support from the NSF award EAR2022716.
Data Availability
The BPRs data of NEPTUNE used in this study were collected from the Incorporated Research Institutions for Seismology (IRIS) Data Management Center (DMC; https://ds.iris.edu/mda/NV/). The DART data are from National Oceanic and Atmospheric Administration (NOAA, https://www.ngdc.noaa.gov/thredds/catalog/dart_bpr/processed/catalog.html). The tide gauge data 9419750 at Crescent City is also NOAA but in a different website (https://tidesandcurrents.noaa.gov/waterlevels.html?id=9419750). The bathymetry data is downloaded from https://www.gebco.net/data_and_products/gridded_bathymetry_data/. All data needed to evaluate the conclusions in the paper are present in the paper and/or the Supporting Information S1. Three days of DAS data including the tsunami and infragravity waves shown in Figures 2-4 are accessible on Zenodo (Spica et al., 2023; Xiao & Spica, 2024).
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Additional details
- ISSN
- 1944-8007
- Gordon and Betty Moore Foundation
- 9500
- National Science Foundation
- EAR-1848166
- National Science Foundation
- EAR-2022716
- Caltech groups
- Division of Geological and Planetary Sciences, Seismological Laboratory