Manifestation of the 2025 Kamchatka Tsunami on the Shumshu Island Coast (Northern Kuriles): Field Surveys and Numerical Simulations

А. I. Zaytsev1, 2, ✉, E. N. Pelinovsky2, 3, I. S. Kostenko1, А. О. Tsepkalo4

1 Special Research Bureau for Automation of Marine Researches (SRB AMR), FEB RAS, Yuzhno-Sakhalinsk, Russian Federation

2 A. V. Gaponov-Grekhov Institute of Applied Physics, Russian Academy of Sciences, Nizhny Novgorod, Russian Federation

3 National Research Universiy – Higher School of Economics, Nizhny Novgorod, Russian Federation

4 Regional Branch of RPM “Search Movement of Russia”, Yuzhno-Sakhalinsk, Russian Federation

e-mail: aizaytsev@mail.ru

Abstract

Purpose. The purpose of this study is to investigate the parameters of the Kamchatka tsunami induced by the earthquake of July 29 (30), 2025, off the Kamchatka Peninsula, and its manifestations on the northern coast of Shumshu Island (Northern Kuril Islands), based on field survey results and numerical simulations.

Methods and Results. The results of field surveys of tsunami deposits in the northern part of Shumshu Island made it possible to determine the boundaries of maximum penetration of tsunami waves into the island interior and to measure the run-up heights at eight points. The coordinates of the maximum inundation line were recorded by GPS, and the run-up heights were determined using the Gebco_2019 Grid topographic maps. Wave generation, propagation, and run-up were numerically simulated within the framework of shallow water theory using the NAMI DANCE software package and nested grids with a minimum grid size of 8 m in the coastal zone. It was established that on the northern (Sea of Okhotsk) coast of Shumshu Island, the average run-up heights were 3–4 m and the maximum reached 6 m, whereas on the eastern (Pacific Ocean) coast of the island, they were 6–8 m, and the maximum in the Cape Pochtarev area reached 12 m (with wave penetration inland up to 110 m). It was shown that significant tsunami-induced fluctuations in sea level occurred not only off the Pacific coast of Shumshu Island on the side of the tsunami source, but also in the narrow shallow straits (First and Second Kuril Straits) separating the island from the Kamchatka Peninsula and Paramushir Island.

Conclusions. The results of numerical simulations are in good agreement with the field survey data, which confirms the reliability of the performed simulations and the possibility of applying the approach used to assess the tsunami hazard in the region. The resulting run-up heights (up to 12 m) indicate the extreme nature of the tsunami.

Keywords

earthquake, Kamchatka, Kuril Islands, tsunami, field survey, numerical simulation

Acknowledgements

The presented results were obtained within the framework of Russian Science Foundation grant No. 25-27-00367.

About the authors

Andrey I. Zaytsev, Leading Researcher, Special Research Bureau for Automation of Marine Researches, FEB RAS (25 Gorky Str., Yuzhno-Sakhalinsk, 693023, Russian Federation), DSc. (Phys.-Math.), ORCID ID: 0000-0002-1383-363X, ResearcherID: A-1772-2014, SPIN-code: 5187-0925, aizaytsev@mail.ru

Efim N. Pelinovsky, Chief Researcher, A. V. Gaponov-Grekhov Institute of Applied Physics, Russian Academy of Sciences (46 Ulyanov Str., Nizhny Novgorod, 603950, Russian Federation), DSc. (Phys.-Math.), Professor, ORCID ID: 0000-0002-5092-0302, ResearcherID: I-3670-2013, SPIN-code: 8949-9088, pelinovsky@gmail.com

Irina S. Kostenko, Senior Researcher, Special Research Bureau for Automation of Marine Researches, FEB RAS (25 Gorky Str., Yuzhno-Sakhalinsk, 693023, Russian Federation), CSc. (Phys.-Math.), ORCID ID: 0009-0008-8630-1555, ResearcherID: A-3142-2014, SPIN-code: 2028-1116, i.kostenko@skbsami.ru

Anna O. Tsepkalo, Regional Branch of RPM “Search Movement of Russia” (132 Pobedy Ave., Yuzhno-Sakhalinsk, 693008, Russian Federation), Tsepkalo.y.s@gmail.com

Original russian text

Original Russian Text © The Authors, 2026, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 42, Iss. 2, pp. 263–274 (2026)

For citation

Zaytsev, A.I., Pelinovsky, E.N., Kostenko, I.S. and Tsepkalo, A.O., 2026. Manifestation of the 2025 Kamchatka Tsunami on the Shumshu Island Coast (Northern Kuriles): Field Surveys and Numerical Simulations. Physical Oceanography, 33(2), pp. 307-318.

References

  1. Benz, H., Herman, M., Furlong, K., Jones, E., Schmitt, R., Yeck, W. and Barnhart, W., 2025. The 29 July 2025, M 8.8 Kamchatka Earthquake. U.S. Geological Survey StoryMap. Available at: https://storymaps.arcgis.com/stories/605361fadf4548e5883d309fb79e1188 [Accessed: 18 March 2026].
  2. Omira, R., Dogan, G.G., Hidayat, R., Husrin, S., Prasetya, G., Annunziato, A., Proietti, C., Probst, P., Paparo, M.A. [et al.], 2019. The September 28th, 2018, Tsunami in Palu-Sulawesi, Indonesia: A Post-Event Field Survey. Pure and Applied Geophysics, 176(4), pp. 1379-1395. https://doi.org/10.1007/s00024-019-02145-z
  3. Zaytsev, A.I., Kostenko, I.S., Kurkin, A.A. and Pelinovsky, E.N., 2016. Tsunami on Sakhalin Island: Observation and Numerical Simulation. Nizhny Novgorod, 121 p. (in Russian).
  4. Kostenko, I.S., Zaytsev, A.I. and Pelinovsky, E.N., 2025. Tsunami on July 29 (30), 2025 in the Kamchatka-Kuril Zone: Instrumental Observation and Modeling. Doklady Earth Sciences, 525(2), 30. https://doi.org/10.1134/S1028334X25608648
  5. Levin, B.W. and Nosov, M.A., 2009. Physics of Tsunamis. Dordrecht: Springer, 327 p.
  6. Okada, Y., 1985. Surface Deformation Due to Shear and Tensile Faults in a Half-Space. Bulletin of the Seismological Society of America, 75(4), pp. 1135-1154. https://doi.org/10.1785/BSSA0750041135
  7. Zaytsev, A., Kurkin, A., Pelinovsky, E. and Yalciner, A.C., 2019. Numerical Tsunami Model NAMI-DANCE. Science of Tsunami Hazards, 38(4), pp. 151-168.
  8. Dogan, G.G., Annunziato, A., Hidayat, R., Husrin, S., Prasetya, G., Kongko, W., Zaytsev, A., Pelinovsky, E., Imamura, F. [et al.], 2021. Numerical Simulations of December 22, 2018 Anak Krakatau Tsunami and Examination of Possible Submarine Landslide Scenarios. Pure and Applied Geophysics, 178(1), pp. 1-20. https://doi.org/10.1007/s00024-020-02641-7
  9. Zayakin, Yu.A., 1996. Tsunami in the Far East of Russia. Petropavlovsk-Kamchatsky: Kamshat, 88 p. (in Russian).
  10. Kaistrenko, V. and Sedaeva, V., 2001. 1952 North Kuril Tsunami: New Data from Archives. In: G.T. Hebenstreit, ed., 2001. Tsunami Research at the End of a Critical Decade. Advances in Natural and Technological Hazards Research, vol. 18. Dordrecht: Springer, pp. 91-102. https://doi.org/10.1007/978-94-017-3618-3_8
  11. Shevchenko, G.V., Ivelskaya, T.N. and Kaistrenko, V.M., 2012. [Tsunami in the Kuril Islands. Characteristics and Risk Mitigation Measures (Dedicated to the Memory of the Victims of the Tragedy of November 5, 1952)]. Yuzhno-Sakhalinsk: IMGG FEB RAS, 44 p. (in Russian).

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