Japan Geoscience Union Meeting 2016

Presentation information


Symbol S (Solid Earth Sciences) » S-VC Volcanology

[S-VC47] Active volcanism

Wed. May 25, 2016 9:00 AM - 10:30 AM Convention Hall B (2F)

Convener:*Yosuke Aoki(Earthquake Research Institute, University of Tokyo), Yuta Maeda(Nagoya University), Chair:Mie Ichihara(Earthquake Research Institute, University of Tokyo), Akimichi Takagi(Volcanology Research Department, Meteorological Research Institute)

9:30 AM - 9:45 AM

[SVC47-15] Volcanic activity of the Nishinoshima volcano detected by ocean bottom seismometers and remote sensing observations

*Akimichi Takagi1, Yutaka Nagaoka1, Azusa Nishizawa2, Tomozo Ono2, Kenji Nakata3, Kazuhiro Kimura3, Keiichi Fukui1, Shinobu Ando3, Hiroaki Tsuchiyama4 (1.Volcanology Research Department, Meteorological Research Institute, 2.Hydrographic and Oceanographic Department, Japan Coast Guard, 3.Seismology and Tsunami Research Department, Meteorological Research Institute, 4.Seismology and Volcanology Department, Japan Meteorological Agency)

Keywords:Nishinoshima, ocean bottom seismometer, monochromatic earthquake, remote sensing

In order to detect seismic activity of the Nishinoshima Island volcano which continues to eruptions actively, the network of self-popup-type ocean-bottom seismometers (OBS) was deployed around the island by the Meteorological Research Institute. We report the brief summary of the seismic activity of Nishinoshima with reference to other remote sensing observations.
Five observation devices which have one three-component seismometer and one hydrophone were installed 4 - 5 km far from the center of Nishinoshima Island, and recorded seismic activity from June 12 to October 2, 2015. This observation revealed that micro-earthquake activity around Nishinoshima volcano was so active. Many micro earthquakes were estimated to be M -1 - 0. Duration time of waveform is around 30 seconds, and envelope of waveform is spindle shape without clear P and S phases. Initial part of waveform has high-frequency component. In later part, the low-frequency component is dominant. Hourly number of recorded waveform was 50 - 100 during the period of OBS. The number of waveforms was around 100 in June, 2015. But seismicity began to weaken in August, and then the number reached to 40 per hour in October. Amplitude of waveform has reached a large size gradually.
The gradual decrease trend of seismicity was consistent with variance of brightness temperature monitored by JMA’s geostationary meteorological satellite Himawari-8 (JMA, 2016). In addition, though SO2 flux in volcanic plume was measured to be 900 ton per day in May, 2015 by the Differential Optical Absorption Spectroscopy (DOAS), decreased to 400 ton per day in October, 2015. Moreover, heat flux of plume by optical sensor on the artificial satellite has decreased, and also incoherent area of the volcanic island by satellite SAR has decreased. So the gradual decrease trend of seismicity must have been synchronized to thermal and gas-emission activity in Nishinoshima volcano.
Another OBS network had been deployed around Nishinoshima from June 25 to July 5, 2015 by Japan Coast Guard (JCG). OBS station St5, located 8 km south far from Nishinoshima, detected active seismic swarms of monochromatic earthquakes. These waveforms have steep dominant frequency of 9 – 10Hz, and decays slowly. All of waveform oscillations have same direction, and b value, estimated from frequency distribution of seismic scale, was calculated to be 1.3. St5, recorded these waveforms, was located near submarine volcano Nishinoshima-Minami Knoll. Around this area, discolored seawater and/or thermal anomaly were observed until now. Therefore this monochromatic-earthquakes swarm may have been recorded as an original volcanic activity different from Nishinoshima volcano.

Keifu Maru, the marine weather observation ship managed by Global Environment and Marine Department, JMA, was used for installation and pickup of OBS.