Abstract
Ray tracing, which has been widely used for seismic waves, was also applied to tsunamis to examine the bathymetry effects during propagation, but it was limited to linear shallow-water waves. Green’s law, which is based on the conservation of energy flux, has been used to estimate tsunami amplitude on ray paths. In this study, we first propose a new ray tracing method extended to dispersive tsunamis. By using an iterative algorithm to map two-dimensional tsunami velocity fields at different frequencies, ray paths at each frequency can be traced. We then show that Green’s law is valid only outside the source region and that extension of Green’s law is needed for source amplitude estimation. As an application example, we analyzed tsunami waves generated by an earthquake that occurred at a submarine volcano, Smith Caldera, near Torishima, Japan, in 2015. The ray-tracing results reveal that the ray paths are very dependent on its frequency, particularly at deep oceans. The validity of our frequency-dependent ray tracing is confirmed by the comparison of arrival angles and travel times with those of observed tsunami waveforms at an array of ocean bottom pressure gauges. The tsunami amplitude at the source is nearly twice or more of that just outside the source estimated from the array tsunami data by Green’s law.
Similar content being viewed by others
References
Abe, K. (1973). Tsunami and mechanism of great earthquakes. Physics of the Earth and Planetary Interiors, 7, 143–153. https://doi.org/10.1016/0031-9201(73),90005-8.
Aki, K., & Richards, P. G. (1980). Quantitative seismology: Theory and methods. New York: W. H. Freeman.
Arfken, G. B., Weber, H. J., & Harris, F. E. (2012). Mathematical methods for physicists: A comprehensive guide (7th ed.). Waltham: Academic Press. https://doi.org/10.1016/b978-0-12-384654-9.00031-1.
Baba, T., Cummins, P., Thio, H., & Tsushima, H. (2009). Validation and joint inversion of teleseismic waveforms for earthquake source models using deep ocean bottom pressure records: A case study of the 2006 Kuril megathrust earthquake. Pure Applied Geophysics, 166(1–2), 55–76. https://doi.org/10.1007/s00024-008-0438-1.
Carrier, G. F., & Yeh, H. (2005). Tsunami propagation from a finite source. COMPUTER MODELING IN ENGINEERING AND SCIENCES, 10(2), 113. http://www.techscience.com/doi/10.3970/cmes.2005.010.113.pdf.
Červený, V. (2001). Seismic ray theory. Cambridge: Cambridge University Press. https://doi.org/10.1017/cbo9780511529399.
Dingemans, M. W. (1997). Water wave propagation over uneven bottoms, part 1, linear wave propagation (vol. 13). Advanced series on ocean engineering. River Edge: World Science Publishing.
Fukao, Y., & Furumoto, M. (1975). Mechanism of large earthquakes along the eastern margin of the Japan Sea. Tectonophysics, 26, 247–266. https://doi.org/10.1016/0040-1951(75),90093-1.
Fukao, Y., Sugioka, H., Ito, A., Shiobara, H., Sandanbata, O., Watada, S., & Satake K. (2016). 2015 Volcanic tsunami earthquake near Torishima island: Array analysis of ocean bottom pressure gauge records. Abstract [NH43B-1853] Presented at 2016 Fall Meeting, AGU, San Francisco, CA, 12–16 Dec.
Glimsdal, S., Pedersen, G., Atakan, K., Harbitz, C. B., Langtangen, H. P., & Lovholt, F. (2006). Propagation of the Dec. 26, 2004, Indian Ocean Tsunami: Effects of dispersion and source characteristics. International Journal of Fluid Mechanics Research, 33(1), 15–43. https://doi.org/10.1615/interjfluidmechres.v33.i1.30.
Glimsdal, S., Pedersen, G., Harbitz, C., & Løvholt, F. (2013). Dispersion of tsunamis: Does it really matter? Natural Hazards and Earth Systems Sciences, 13, 1507–1526.
Hossen, M., Cummins, P., Dettmer, J., & Baba, T. (2015). Tsunami waveform inversion for sea surface displacement following the 2011 Tohoku earthquake: Importance of dispersion and source kinematics. Journal of Geophysical Research: Solid Earth, 120(9), 6452–6473. https://doi.org/10.1002/2015JB011942.
Julian, B. R., (1970). Ray tracing in arbitrarily homogeneous media, Technical Note 1970-45, Lincoln Laboratory, Massachusetts Institute of Technology.
Kajiura, K. (1970). Tsunami source, energy and the directivity of wave radiation. Bull. Earthq. Res. Inst. Univ. 48, 835–869. http://ci.nii.ac.jp/naid/120000871347/.
Kanamori, H. (1972). Mechanisms for tsunami earthquakes. Physics of the Earth and Planetary Interiors, 6, 346–359. https://doi.org/10.1016/0031-9201(72),90058-1.
Kanamori, H., Ekström, G., Dziewonski, A., Barker, J. S., & Sipkin, S. A. (1993). Seismic radiation by magma injection: An anomalous seismic event near Tori Shima, Japan. Journal of Geophysical Research, 98(B4), 6511–6522. https://doi.org/10.1029/92JB02867.
Kervella, Y., Dutykh, D., & Dias, F. (2007). Comparison between three-dimensional linear and nonlinear tsunami generation models. Theoretical and computational fluid dynamics, 21(4), 245–269. https://doi.org/10.1007/s00162-007-0047-0.
Lamb, H. (1932). Hydrodynamics (6th ed.). Cambridge: Cambridge University Press.
Lin, F.-C., Kohler, M. D., Lynett, P., Ayca, A., & Weeraratne, D. S. (2015). The 11 March 2011 Tohoku tsunami wavefront mapping across offshore Southern California. Journal of Geophysical Research: Solid Earth, 120, 3350–3362. https://doi.org/10.1002/2014JB011524.
Murty, T. S. (1977). seismic sea waves—tsunamis. Ottawa: Department of Fisheries and Environment.
Officer, C. B. (1974). Introduction to theoretical geophysics. New York: Springer.
Piessens, R. (2000). The Hankel transform, the transforms and applications handbook (2nd ed.). Boca Raton: CRC Press. https://doi.org/10.1201/9781420036756.ch9.
Saito, T., Satake, K., & Furumura, T. (2010). Tsunami waveform inversion including dispersive waves: The 2004 earthquake off Kii Peninsula, Japan. Journal of Geophysical Research, 115, B06303. https://doi.org/10.1029/2009JB006884.
Satake, K. (1987). Inversion of tsunami waveforms for the estimation of a fault heterogeneity: Method and numerical experiments. Journal of Physics of the Earth, 35(3), 241–254. https://doi.org/10.4294/jpe1952.35.241.
Satake, K. (1988). Effects of bathymetry on tsunami propagation: Application of ray tracing to tsunamis. Pure and Applied Geophysics, 126(1), 27–36. https://doi.org/10.1007/BF00876912.
Shearer, P. (1999). Introduction to seismology. Cambridge: Cambridge University Press.
Shuler, A., Ekström, G., & Nettles, M. (2013a). Physical mechanisms for vertical-CLVD earthquakes at active volcanoes. Journal of Geophysical Research: Solid Earth, 118, 1569–1586. https://doi.org/10.1002/jgrb.50131.
Shuler, A., Nettles, M., & Ekström, G. (2013b). Global observation of vertical-CLVD earthquakes at active volcanoes. Journal of Geophysical Research: Solid Earth, 118, 138–164. https://doi.org/10.1029/2012JB009721.
Tappin, D. R., Grilli, S. T., Harris, J. C., Geller, R. J., Masterlark, T., Kirby, J. T., et al. (2014). Did a submarine landslide contribute to the 2011 Tohoku tsunami? Marine Geology, 357(1), 344–361. https://doi.org/10.1016/j.margeo.2014.09.043.
Watada, S. (2013). Tsunami speed variations in density–stratified compressible global oceans. Geophysical Research Letters, 40, 4001–4006. https://doi.org/10.1002/grl.50785.
Wiegel, R. L. (1970). Earthquake Engineering. Englewood Cliffs: Prentice-Hall.
Wielandt, E. (1993). Propagation and structural interpretation of nonplane waves. Geophysical Journal International, 113, 45–53. https://doi.org/10.1111/j.1365-246X.1993.tb02527.x.
Witting, J. M. (1981). A note on Green’s law. Journal of Geophysical Research, 86(C3), 1995–1999. https://doi.org/10.1029/JC086iC03p01995.
Woods, M., & Okal, E. (1987). Effect of variable bathymetry on the amplitude of teleseismic tsunamis: A ray–tracing experiment. Geophysical Research Letters. https://doi.org/10.1029/GL014i007p00765.
Yomogida, K., & Aki, K. (1985). Waveform synthesis of surface waves in a laterally heterogeneous Earth by the Gaussian Beam Method. Journal of Geophysical Research, 90(B9), 7665–7688. https://doi.org/10.1029/JB090iB09p07665.
Acknowledgements
We used the bathymetry data, JTOPO30, provided by the Marine Information Research Center of the Japan Hydrographic Association. The earthquake information data are obtained from the Global Centroid Moment Tensor catalog. The information of tsunami at Hachijo Island is reported in Japanese by Japan Meteorological Agency (http://www.jma.go.jp/jma/press/1505/13a/1504recently-eq.pdf). We generated figures with the Generic Mapping Tools (GMT) data processing and package and Gnuplot. We also used Mathematica to analyze and plot the solutions of the wave equations. The simulation parts are supported by the JSPS KAKENHI Grant number JP17J02919. The observation was supported by JSPS KAKENHI Grant number 25247074. We appreciate to T. Maeda, R. Geller and T. Furumura for providing valuable comments. We thank four anonymous reviewers whose comments helped us to improve our paper.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Sandanbata, O., Watada, S., Satake, K. et al. Ray Tracing for Dispersive Tsunamis and Source Amplitude Estimation Based on Green’s Law: Application to the 2015 Volcanic Tsunami Earthquake Near Torishima, South of Japan. Pure Appl. Geophys. 175, 1371–1385 (2018). https://doi.org/10.1007/s00024-017-1746-0
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00024-017-1746-0