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Temporal variability of tsunami arrival detection distance revealed by virtual tsunami observation experiments using numerical simulation and 1-month HF radar observation

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Abstract

The combination of a high-frequency ocean surface radar and a tsunami detection method should be assessed as the onshore-offshore distribution of tsunami detection probability, because the probability will vary in accordance with the signal-to-noise ratio (SNR) and the tsunami magnitude in addition to the radar system specifications. Here, we statistically examine the tsunami detection distance based on virtual tsunami observation experiments by using signals received by a high-frequency radar in February 2014 installed on the southern coast of Japan and numerically simulated velocities induced by a Nankai Trough earthquake. In the experiments, the Doppler frequencies associated with the simulated velocities were superimposed on the receiving signals of the radar, and the radial velocities were calculated from the synthesized signals by the fast Fourier transform. Tsunami arrival was then detected based on the temporal change in the cross-correlation of the velocities, before and after tsunami arrival, between two points 3 km apart along a radar beam. We found that the possibility of tsunami detection primarily depends on the kinetic energy ratio between tsunami current and background current velocities. The monthly average detection probability is over 90% when the energy ratio exceeds 5 (offshore distance: 9 km ≤ L ≤ 36 km) and reduces to 50% when the energy ratio is approximately 1 (L = 42 km) over the shelf slope. The ratio varied with the background current physics and SNR, which was mainly affected by ocean surface wave heights and ionospheric electron density.

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Acknowledgements

This research was supported by a collaborative research project between Ehime University and Kokusai Kogyo Co., Ltd., the Mitsubishi Foundation, JSPS Grant-in-Aid for Scientific Research (KAKENHI) number 16H04419, and MIC/SCOPE grant number 165011003. We are grateful to Dr. Takahashi and Dr. Fujii for helpful discussions.

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Correspondence to Ryotaro Fuji.

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Fuji, R., Hinata, H. Temporal variability of tsunami arrival detection distance revealed by virtual tsunami observation experiments using numerical simulation and 1-month HF radar observation. J Oceanogr 73, 725–741 (2017). https://doi.org/10.1007/s10872-017-0428-y

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  • DOI: https://doi.org/10.1007/s10872-017-0428-y

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