Abstract
Although infrequent, volcanic tsunamis have accounted for almost 20% of those killed by volcanic eruptions since 1000 A.D (Mastin and Witter in J Volcanol Geotherm Res 97(1–4):195–214. https://doi.org/10.1016/S0377-0273(99)00174-2, 2000; Latter in Bull Volcanol 44(3):467–490. https://doi.org/10.1007/BF02600578, 1981). The destructive potential and unpredictability of such waves highlight the need to improve our understanding of the phenomena. Underwater eruptions are one of the source mechanisms that can generate volcanic tsunamis. For example, the 1952 explosions of Myojinsho volcano which destroyed a surveying boat of the Japan Hydrographic Department, killing 31 people, also generated a series of tsunamis. Wave gauges at Hachijo Island, 130 km from the volcano, recorded waves of up to 92 cm, which provide us with one of the few wave gauge observations of a tsunami generated by a volcanic eruption. The present work is based on the mathematical model of Duffy (J Volcanol Geotherm Res 50(3):323–344. https://doi.org/10.1016/0377-0273(92)90100-R, 1992), who analysed surface waves generated by an instantaneous underwater point-source volcanic explosion. We extend this work by modifying the source model to include time dependence and compare the efficiency of wave generation of the following sources: the instantaneous source used by Duffy (1992), a source with exponentially decreasing intensity of the explosion, and two time-constrained sources—a source with a defined sharp end to the explosion, and a source that ceases with a cavity at the free surface. The shorter the characteristic time of the exponential explosion, the more like the original Duffy model the resulting waves are. Waves resulting from time-constrained explosions exhibit a beating behaviour. The duration of the explosion modulates the generated wave field while the average wave amplitudes remain the same. Conversely, the geometric parameters of the explosion affect the wave amplitudes. The beating behaviour of our second time-constrained model bears a strong resemblance to that observed in tsunami records from the 1952 Myojinsho explosions. Thus, we apply the model to these events. The predicted leading wave is absent in the recorded data, but the trailing waves were calculated accurately, particularly in terms of the wave phasing and the lengths of the wave groups. We infer that the absence of this leading wave could be due to the mathematical formulation of the problem and it reflects how gas-rich explosions produce sea-surface displacements. The results suggest that the beating behaviour observed in the wave gauges records could have been a consequence of time constraints on the duration of a volcanic explosion.
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Abbreviations
- r :
-
Radial coordinate
- z :
-
Vertical coordinates
- \({\mathbf {u}}\) :
-
Velocity field
- \(\phi \) :
-
Velocity potential
- \(\psi \) :
-
Displacement potential
- t :
-
Time
- \(\delta ( )\) :
-
The Dirac delta function
- \(\phi _0(t)\) :
-
Source strength as a function of time
- \(\eta \) :
-
Free surface elevation
- d :
-
Water depth
- g :
-
Gravitational acceleration
- \(r_0\) :
-
Vent size
- \(z_0\) :
-
Depth of the explosion
- \(S_0\) :
-
Amplitude of the displacement source
- V :
-
Volume of the explosion
- S(r, t):
-
Source function
- G(r, z, t):
-
The Green’s function
- k :
-
Wave number; Hankel-transformed r coordinate
- p :
-
Laplace-transformed t variable
- H( ):
-
The Heaviside step function
- \(\omega \) :
-
Angular frequency
- \(J_0\) :
-
The Bessel function of the first kind of order 0
- \(J_1\) :
-
The Bessel function of the first kind of order 1
- \(\alpha \) :
-
Parameter describing time-scale of the exponential source
- T :
-
Duration of the explosion
References
Airy, G. B. (1841). art. Tides and waves. In H. J. Rose (Ed.), Encyclopedia Metropolitana (1817–1845), Mixed Sciences, London (p. 396, vol. 3 edn).
Belousov, A., & Belousova, M. (2001). Eruptive process, effects and deposits of the 1996 and the ancient basaltic phreatomagmatic eruptions in Karymskoye Lake, Kamchatka, Russia. International Association of Sedimentologists Special Publication, 30, 35–60.
Belousov, A., Voight, B., Belousova, M., & Muravyev, Y. (2000). Tsunamis generated by subaquatic volcanic explosions: Unique data from 1996 Eruption in Karymskoye Lake, Kamchatka, Russia. Pure and Applied Geophysics, 157(6–8), 1135–1143. https://doi.org/10.1007/s000240050021.
Cooke, R. J. S. (1981). Eruptive history of the volcano at Ritter Island. Geological Survey of Papua New Guinea (Memoir), 10, 115–123.
Craig, B. (1974). Experimental Observations of Underwater Detonations Near the Water Surface. Tech. rep., Los Alamos Scientific Laboratory of the University of California (report LA- 5548-MS, UC-34).
Craik, A. D. (2004). The origins of water wave theory. Annual Review of Fluid Mechanics, 36(1), 1–28. https://doi.org/10.1146/annurev.fluid.36.050802.122118.
Dietz, R. S., & Sheehy, M. J. (1954). Transpacific detection of Myojin volcanic explosions by underwater sound. Geological Society of America Bulletin, 65(10), 941–956. https://doi.org/10.1130/0016-7606(1954)65[941:TDOMVE]2.0.CO;2.
Duffy, D. G. (1992). On the generation of oceanic surface waves by underwater volcanic explosions. Journal of Volcanology and Geothermal Research, 50(3), 323–344. https://doi.org/10.1016/0377-0273(92)90100-R.
Egorov, Y. (2007). Tsunami wave generation by the eruption of underwater volcano. Natural Hazards and Earth System Science, 7(1), 65–69. https://doi.org/10.5194/nhess-7-65-2007.
Falvard, S., Paris, R., Belousova, M., Belousov, A., Giachetti, T., & Cuven, S. (2018). Scenario of the 1996 volcanic tsunamis in Karymskoye Lake, Kamchatka, inferred from X-ray tomography of heavy minerals in tsunami deposits. Marine Geology, 396(2016), 160–170. https://doi.org/10.1016/j.margeo.2017.04.011.
Fazlullin, S. M., Ushakov, S. V., Shuvalov, R. A., Aoki, M., Nikolaeva, A. G., & Lupikina, E. G. (2000). The 1996 subaqueous eruption at Academii Nauk volcano (Kamchatka) and its effects on Karymsky lake. Journal of Volcanology and Geothermal Research, 97(1–4), 181–193. https://doi.org/10.1016/S0377-0273(99)00160-2.
Fiske, R. S., Cashman, K. V., Shibata, A., & Watanabe, K. (1998). Tephra dispersal from Myojinsho, Japan, during its shallow submarine eruption of 1952–1953. Bulletin of Volcanology, 59(4), 262–275. https://doi.org/10.1007/s004450050190.
Global Volcanism Program. (2013). Myojinsho (284070). In E. Venzke (Ed.), Volcanoes of the World, v. 4.8.5. Smithsonian Institution. Accessed 12 Jan 2020. https://volcano.si.edu/volcano.cfm?vn=284070. https://doi.org/10.5479/si.GVP.VOTW4-2013.
Goto, A., Taniguchi, H., Yoshida, M., Ohba, T., & Oshima, H. (2001). Effects of explosion energy and depth to the formation of blast wave and crater: Field explosion experiment for the understanding of volcanic explosion. Geophysical Research Letters, 28(22), 4287–4290. https://doi.org/10.1029/2001GL013213.
Hammack, J. L. (1973). A note on tsunamis: Their generation and propagation in an ocean of uniform depth. Journal of Fluid Mechanics, 60(4), 769–799. https://doi.org/10.1017/S0022112073000479.
Kajiura, K. (1963). The leading waves of tsunami. Bulletin of the Earthquake Research Institute, 41, 535–571.
Kedrinskiy, V. (2005). Hydrodynamics of explosion. Berlin: Springer.
Kranzer, H. C., & Keller, J. B. (1959). Water waves produced by explosions. Journal of Applied Physics, 30(3), 398–407. https://doi.org/10.1063/1.1735176.
Lamb, H. (1922). On water waves due to disturbances beneath the surface. Proceedings of the London Mathematical Society, 2(21), 359–372. https://doi.org/10.1112/plms/s2-21.1.359.
Latter, J. (1981). Tsunamis of volcanic origin: Summary of causes, with particular reference to Krakatoa, 1883. Bulletin Volcanologique, 44(3), 467–490. https://doi.org/10.1007/BF02600578.
Le Mehaute, B., & Wange, B. (1996). Water waves generated by underwater explosions. Advanced series on ocean engineering (Vol. 10). New Jersey: World Scientific.
Le Mehaute, B. (1971). Theory of explosion-generated waves. In Advances in hydroscience (Vol. 7). New York, NY: Academic Press.
Lyons, J. J., Haney, M. M., Fee, D., Wech, A. G., & Waythomas, C. F. (2019). Infrasound from giant bubbles during explosive submarine eruptions. Nature Geoscience, 12(11), 952–958. https://doi.org/10.1038/s41561-019-0461-0.
Mastin, L., & Witter, J. (2000). The hazards of eruptions through lakes and seawater. Journal of Volcanology and Geothermal Research, 97(1–4), 195–214. https://doi.org/10.1016/S0377-0273(99)00174-2.
MATLAB. (2018). MATLAB version 9.5.0.944444 (R2018b). Natick: The Mathworks, Inc.
Mirchina, N. R., & Pelinovsky, E. N. (1988). Estimation of underwater eruption energy based on tsunami wave data. Natural Hazards, 1(3), 277–283. https://doi.org/10.1007/BF00137232.
Miyoshi, H., & Akiba, Y. (1954). The tsunamis caused by the Myojin explosions. Journal of the Oceanographic Society of Japan, 10(2), 49–59.
Moore, J. G., Nakamura, K., & Alcaraz, A. (1966). The September 28–30, 1965 eruption of Taal Volcano, Philippines. Bulletin Volcanologique, 29(1), 75–76. https://doi.org/10.1007/BF02597143.
Morimoto, R., & Osaka, J. (1955). The 1952–1953 submarine eruption of the Myojin Reef near the Bayonnaise Rocks, Japan. Bulletin of the Earthquake Research Institute, Tokyo University, 33(2), 221–250.
Morrissey, M., Gisler, G., Weaver, R., & Gittings, M. (2010). Numerical model of crater lake eruptions. Bulletin of Volcanology, 72(10), 1169–1178. https://doi.org/10.1007/s00445-010-0392-5.
Muravyev, Y., Fedotov, S., Budnikov, V., Ozerov, A., Maguskin, M., Dvigalo, V., et al. (1998). Activity in the karymsky center in 1996: Summit eruption at karymsky and phreatomagmatic eruption in the akademii nauk caldera. Volcanology and Seismology, 19(5), 567–604.
Nakano, M., Unoki, S., Hanzawa, M., Marumo, R., & Fukuoka, J. (1954). Oceanographic features of a submarine eruption that destroyed the Kaiyo-Maru No. 5. Journal of Marine Research, 13(1), 48–66.
Nishimura, Y., Nakagawa, M., Kuduon, J., & Wukawa, J. (2005). Timing and scale of tsunamis caused by the 1994 Rabaul Eruption, East New Britain, Papua New Guinea (pp. 43–56). Dordrecht: Springer Netherlands. https://doi.org/10.1007/1-4020-3331-1_3.
Paris, R. (2015). Source mechanisms of volcanic tsunamis. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 373(2053), 1–15. https://doi.org/10.1098/rsta.2014.0380.
Paris, R., & Ulvrová, M. (2019). Tsunamis generated by subaqueous volcanic explosions in Taal Caldera Lake, Philippines. Bulletin of Volcanology, 81(3), 14. https://doi.org/10.1007/s00445-019-1272-2.
Paris, R., Ulvrová, M., Selva, J., Brizuela, B., Costa, A., Grezio, A., et al. (2019). Probabilistic hazard analysis for tsunamis generated by subaqueous volcanic explosions in the Campi Flegrei caldera, Italy. Journal of Volcanology and Geothermal Research, 379, 106–116. https://doi.org/10.1016/j.jvolgeores.2019.05.010.
Pease, R. (2019). Ship spies newborn underwater volcano. Science, 364(6442), 720. https://doi.org/10.1126/science.aay1175.
Raue, H. (2004). A new model for the fracture energy budget of phreatomagmatic explosions. Journal of Volcanology and Geothermal Research, 129(1), 99–108. https://doi.org/10.1016/S0377-0273(03)00234-8.
Ross, P. S., White, J. D. L., Zimanowski, B., & Büttner, R. (2008). Rapid injection of particles and gas into non-fluidized granular material, and some volcanological implications. Bulletin of Volcanology, 70(10), 1151–1168. https://doi.org/10.1007/s00445-008-0230-1.
Sato, H., & Taniguchi, H. (1997). Relationship between crater size and ejecta volume of recent magmatic and phreato-magmatic eruptions: Implications for energy partitioning. Geophysical Research Letters, 24(3), 205–208. https://doi.org/10.1029/96GL04004.
Smith, M. S., & Shepherd, J. B. (1993). Preliminary investigations of the tsunami hazard of Kickem Jenny submarine volcano. Natural Hazards, 7(3), 257–277. https://doi.org/10.1007/BF00662650.
Smith, M. S., & Shepherd, J. B. (1995). Potential Cauchy–Poisson waves generated by submarine eruptions of Kickem Jenny volcano. Natural Hazards, 11(1), 75–94. https://doi.org/10.1007/BF00613311.
Soule, S. A. (2015). Chapter 21—Mid-ocean ridge volcanism. In H. Sigurdsson (Ed.), The encyclopedia of volcanoes (Second Edition) (pp. 395–403). Amsterdam: Academic Press. https://doi.org/10.1016/B978-0-12-385938-9.00021-3.
Speight, M., & Henderson, P. A. (2010). Marine Ecology: Concepts and Applications. Wiley.
Staudigel, H., & Koppers, A. A. (2015). Chapter 22—Seamounts and island building. In H. Sigurdsson (Ed.) The encyclopedia of volcanoes (Second Edition) (pp. 405–421). Amsterdam: Academic Press. https://doi.org/10.1016/B978-0-12-385938-9.00022-5.
Terazawa, K. (1915). On deep-sea water waves caused by a local disturbance on or beneath the surface. Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 92(635), 57–81. https://doi.org/10.1098/rspa.1915.0053.
Torsvik, T., Paris, R., Didenkulova, I., Pelinovsky, E., Belousov, A., & Belousova, M. (2010). Numerical simulation of a tsunami event during the 1996 volcanic eruption in Karymskoye lake, Kamchatka, Russia. Natural Hazards and Earth System Science, 10(11), 2359–2369. https://doi.org/10.5194/nhess-10-2359-2010.
Ulvrová, M., Paris, R., Kelfoun, K., & Nomikou, P. (2014). Numerical simulations of tsunamis generated by underwater volcanic explosions at Karymskoye lake (Kamchatka, Russia) and Kolumbo volcano (Aegean Sea, Greece). Natural Hazards and Earth System Sciences, 14(2), 401–412. https://doi.org/10.5194/nhess-14-401-2014.
Unoki, S., & Nakano, M. (1953). On the Cauchy–Poisson waves caused by the eruption of a submarine volcano (III). Papers in Meteorology and Geophysics, 4, 139–150.
Valentine, G., Graettinger, A., & Sonder, I. (2014). Explosion depths for phreatomagmatic eruptions. Geophysical Research Letters, 41(9), 3045–3051. https://doi.org/10.1002/2014GL060096.
Whalin, R. W. (1965). Water waves produced by underwater explosions: Propagation theory for regions near the explosion. Journal of Geophysical Research, 70(22), 5541–5549. https://doi.org/10.1029/JZ070i022p05541.
White, J. D., McPhie, J., & Soule, S. A. (2015a). Chapter 19—Submarine lavas and hyaloclastite. In H. Sigurdsson (Ed.), The encyclopedia of volcanoes (Second Edition) (pp. 363–375). Amsterdam: Academic Press. https://doi.org/10.1016/B978-0-12-385938-9.00019-5.
White, J. D., Schipper, C. I., & Kano, K. (2015b). Chapter 31—Submarine explosive eruptions. In H. Sigurdsson (Ed.), The encyclopedia of volcanoes (pp. 553–569). Amsterdam: Academic Press. https://doi.org/10.1016/B978-0-12-385938-9.00031-6.
Acknowledgements
This research was funded by the Marsden Fund Council, Royal Society Te Ap\({\bar{a}}\)rangi Grant Number 17-NIW-017 awarded to NIWA.
Funding
This study is a part of a NIWA led project titled: Volcanoes can make waves too: a new understanding of tsunamis generated by volcanic eruptions, funded by the Royal Society of New Zealand Marsden Fund no 17-NIWA-017. Leaders are Emily Lane with William Power as co-PI.
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Lipiejko, N., Whittaker, C.N., Lane, E.M. et al. Tsunami Generation by Underwater Volcanic Explosions: Application to the 1952 Explosions of Myojinsho Volcano. Pure Appl. Geophys. 178, 4743–4761 (2021). https://doi.org/10.1007/s00024-021-02857-1
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DOI: https://doi.org/10.1007/s00024-021-02857-1