EGU2020-3231
https://doi.org/10.5194/egusphere-egu2020-3231
EGU General Assembly 2020
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Recent advances in GNSS-A observation technology and networks and latest observation results around Japan Islands

Yusuke Yokota1, Tadashi Ishikawa2, Shun-ichi Watanabe3, and Yuto Nakamura4
Yusuke Yokota et al.
  • 1Center for Integrated Underwater Observation Technology, Institute of Industrial Science, University of Tokyo, Tokyo, Japan (yyokota@iis.u-tokyo.ac.jp)
  • 2Hydrographic and Oceanographic Department, Japan Coast Guard, Tokyo, Japan (ishikawa@jodc.go.jp)
  • 3Hydrographic and Oceanographic Department, Japan Coast Guard, Tokyo, Japan (s-watanabe@jodc.go.jp)
  • 4Hydrographic and Oceanographic Department, Japan Coast Guard, Tokyo, Japan (ynakamura@jodc.go.jp)

Our research group has been studying advanced GNSS-A (Global Navigation Satellite System – Acoustic ranging combination) technique over two decades. In recent years, detection sensitivity of GNSS-A observations has been sophisticated by improving the accuracy and frequency of analysis technology and acoustic systems [e.g., Yokota et al., 2018, MGR; Ishikawa et al., in prep]. The current observation frequency is more than 4 times/year, the observation accuracy for each observation is less than 2 cm, and it can detect a steady deformation rate of 1 cm/year or less and an unsteady fluctuation of 5 cm or less. Also, efforts are being made to strengthen the observation network.

GNSS-A observations for the 2011 Tohoku-oki earthquake and its postseismic field revealed the details of the crustal deformation field on the Japan Trench side [Sato et al., 2011, Science; Watanabe et al., 2014, GRL]. The long-term observation data in the Nankai Trough region revealed the strain accumulation process at the interseismic period [Yokota et al., 2016, Nature; Watanabe et al., 2018, JGR; Nishimura et al., 2018, Geosphere]. Furthermore, detection and monitoring of large-scale slow slip events (SSEs) in the shallow part of the Nankai Trough was achieved by recent sensitivity improvements [Yokota & Ishikawa, 2020, Science Advances]. The detected postseismic fields, coupling condition and shallow SSEs contain universal features that should be shared in many subduction zones. Here, along with the latest observations, we discuss spatial and temporal relationships of these events, strain accumulations and releases along subduction zones around Japan by GNSS-A and its impact on slow earthquake science.

Recently, because of the need for continuous monitoring a shallow SSE, the monitoring ability of GNSS-A was also investigated. It was confirmed that relatively large-scale shallow SSE (surface deformation: > 5 cm) could be monitored. However, the ability to determine the time constant of an SSE is poor. For monitoring the detail of an SSE, it is essential to improve the observation frequency in the future. Here, we also discuss the technical issues to be considered and their solution plans (e.g., new platform and system).

How to cite: Yokota, Y., Ishikawa, T., Watanabe, S., and Nakamura, Y.: Recent advances in GNSS-A observation technology and networks and latest observation results around Japan Islands, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3231, https://doi.org/10.5194/egusphere-egu2020-3231, 2020.

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