single-dr.php

JDR Vol.13 No.3 pp. 518-525
(2018)
doi: 10.20965/jdr.2018.p0518

Review:

Volcanic Activity of Sakurajima Monitored Using Global Navigation Satellite System

Masato Iguchi

Sakurajima Volcano Research Center, Disaster Prevention Research Institute, Kyoto University
1722-19, Sakurajima-Yokoyama, Kagoshima 891-1419, Japan

Corresponding author

Received:
November 15, 2017
Accepted:
January 28, 2018
Published:
June 1, 2018
Keywords:
GNSS, ground deformation, eruption, Sakurajima volcano
Abstract

A dense Global Navigation Satellite System (GNSS) network has been deployed at Sakurajima volcano since 1995 and extends to the surrounding area of the Aira caldera. The ground deformation obtained by GNSS observation corresponds to transient eruptive activity of Sakurajima volcano, which has produced frequent vulcanian eruptions since 1955. Inflation of the volcano was detected prior to the increase in vulcanian eruptions in 1999, and resumption of the eruptions at the Showa crater. Magma intrusion events and an increase in eruptions in late 2009, late 2011, and early 2015 suggest the existence of an open-conduit system from the Aira caldera to the vents at the summit area of the Minamidake cone, through the sub reservoir beneath the older Kitadake cone. Ground deformation induced by sudden dike intrusion is different from that of previous intrusions, as revealed by the dense GNSS network. GNSS data are useful in evaluating and forecasting volcanic activity, and are available to grasp the advection and diffusion of volcanic ash.

Cite this article as:
M. Iguchi, “Volcanic Activity of Sakurajima Monitored Using Global Navigation Satellite System,” J. Disaster Res., Vol.13, No.3, pp. 518-525, 2018.
Data files:
References
  1. [1] F. Omori, “The Sakura-Jima eruptions and earthquakes,” II. Bull. Imp. Earthq. Inv. Comm., Vol.8, No.6, p. 179, 1916.
  2. [2] K. Mogi, “Relation between the eruptions of various volcanoes and the deformations of the ground surface around them,” Bull. Earthq. Res. Inst., Univ. Tokyo, Vol.36, pp. 99-134, 1958.
  3. [3] K. Yoshikawa, “On the crustal movement accompanying with the recent activity of the volcano Sakurajima (Part 1),” Bull. Disast. Prev. Res. Inst., Kyoto Univ., Vol.48, pp. 1-15, 1961.
  4. [4] K. Ishihara, T. Takayama, Y. Tanaka, and J. Hirabayashi, “Lava flows at Sakurajima volcano (1) Volume of the historical lava flows,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.24, pp. 1-10, 1981. (in Japanese with English abstract)
  5. [5] K. Sassa, “A few problems on prediction of earthquake (II),” In Procs. of the fifth anniversary of founding of Disast. Prev. Res. Inst. Kyoto Univ., pp. 3-7, 1956 (in Japanese).
  6. [6] T. Eto, “Ground deformation at Sakurajima and around Aira caldera associated with the volcanic activity,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.32, pp. 29-39, 1989 (in Japanese with English abstract).
  7. [7] T. Eto, T. Takayama, K. Yamamoto, M. Hendrasto, D. Miki, T. Sonoda, K. Matshushima, K. Uchida, H. Yakiwara, Y. Wan, F. Kimata, R. Miyajima, and K. Kobayashi, “Re-upheaval of the ground surface at the Aira caldera – December 1991 ∼ October 1996 –,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.40B-1, pp. 49-60, 1997 (in Japanese with English abstract).
  8. [8] S. Hidayati, K. Ishihara, and M. Iguchi, “Volcano-tectonic earthquakes during the stage of magma accumulation at the Aira caldera,” southern Kyushu, Japan. Bull. Volcanol. Soc. Japan, Vol.52, pp. 289-309, 2007.
  9. [9] M. Iguchi, T. Tameguri, Y. Ohta, S. Ueki, and S. Nakao, “Characteristics of volcanic activity at Sakurajima volcano’s Showa crater during the period 2006 to 2011,” Bull. Volcanol. Soc. Japan, Vol.58, pp. 115-135, 2013.
  10. [10] K. Hotta, M. Iguchi, and T. Tameguri, “Rapid dike intrusion into Sakurajima volcano on August 15,” 2015, as detected by multi-parameter ground deformation observations, Earth Planets Space, Vol.68, DOI: 10.1186/s40623-016-0450-0, 2016.
  11. [11] T. Eto and S. Nakamura, “Ground deformation around Sakurajima volcano – 1974∼1982 –,” In Report on 5th Joint Observation of Sakurajima Volcano, pp. 11-21, 1986 (in Japanese).
  12. [12] M. Iguchi, T. Takayama, T. Yamazaki, M. Tada, A. Suzuki, S. Ueki, Y. Ohta, and S. Nakao, “Movement of Magma at Sakurajima Volcano Revealed by GPS Observation,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.51B, pp. 241-246, 2008 (in Japanese with English abstract).
  13. [13] E. Kriswati and M. Iguchi, “Inflation of the Aira caldera prior to the 1999 eruptive activity at Sakurajima volcano detected by GPS network in south Kyushu,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.46B, pp. 817-826, 2003.
  14. [14] K. Hotta, M. Iguchi, T. Ohkura, and K. Yamamoto, “Multiple-pressure-source model for ground inflation during the period of high explosivity at Sakurajima volcano, Japan – Combination analysis of continuous GNSS, tilt and strain data –,” J. Volcanol. Geotherm. Res., Vol.310, pp. 12-25, 2016.
  15. [15] Y. Okada, “Internal deformation due to shear and tensile faults in a half space,” Bulletin of the Seismological Society of America, Vol.82, No.2, pp. 1018-1040. 1992.
  16. [16] K. Yamamoto, et al., “Vertical deformation associated with the 15 August 2015 dike intrusion at Sakurajima volcano measured by leveling survey,” Abstracts Japan Geosceince Union Meeting 2016, SVC47-06, 2016.
  17. [17] K. Ishihara and T. Eto, “Surface deformation associated with the eruptive activity at the summit crater of Sakurajima volcano,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.21B-1, pp. 152-162, 1978 (in Japanese with English abstract).
  18. [18] K. Yamashina, “The inflation-deflation history of Aira caldera for past 120 years and the possibility of a forthcoming large eruption at Sakurajima volcano,” Bull. Volcanol. Soc. Japan, Vol.58, pp. 103-114, 2013.
  19. [19] K. Ishihara, “A quantitative relation between the ground deformation and the volcanic materials ejected,” Abstract 1981 IAVCEI Symposium – Arc Volcanism, p. 143, 1981.
  20. [20] J. Hickey, J. Gottsmann, H. Nakamichi, and M. Iguchi, “Thermomechanical controls on magma supply and volcanic deformation: application to Aira caldera,” Japan Scientific Reports, DOI: 10.1038/srep32691, 2016.
  21. [21] M. Maki, M. Iguchi, T. Maesaka, T. Miwa, T. Tanada, T. Kozono, T. Momotani, A. Yamaji, and I. Kakimoto, “Preliminary results of weather radar observations of Sakurajima volcanic smoke,” J. Disaster Res., Vol.11, No.1, pp. 15-30, 2016.
  22. [22] K. Sassen, J. Zhu, P. Webley, K. Dean, and K. Cobb, “Volcanic ash plume identification using polarization lidar: Augustine eruption,” Alaska, Geophys. Res. Lett., Vol.34, L08803, pp. 1-4, 2017.
  23. [23] Y. Ohta and M. Iguchi, “Advective diffusion of volcanic plume captured by dense GNSS network around Sakurajima volcano: a case study of the vulcanian eruption on July 24, 2012,” J. Earth, Planets and Space, 67:157, DOI: 10.1186/s40623-015-0324-x, 2015.
  24. [24] M. Tsukui, “Ash-Fall Distribution of 1779 An’ei Eruption,” Sakurajima Volcano, Bull. Volcanol. Soc. Japan, Ser.2, Vol.56, pp. 89-94, 2011 (in Japanese with English abstract).
  25. [25] K. Yamamoto, S. Yoshikawa, T. Matsushima, T. Ohkura, A. Yokoo, H. Inoue, T. Mishima, K. Uchida, T. Sonoda, K. Seki, S. Komatsu, K. Hotta, and S. Fujita, “Vertical ground deformation in Sakurajima volcano measured by precise leveling survey conducted in November 2014,” Ann. Disast. Prev. Res. Inst., Kyoto Univ., Vol.58B-1, pp. 70-75, 2015 (in Japanese with English abstract).

*This site is desgined based on HTML5 and CSS3 for modern browsers, e.g. Chrome, Firefox, Safari, Edge, IE9,10,11, Opera.

Last updated on Nov. 16, 2018