Japan Geoscience Union Meeting 2021

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-TT Technology & Techniques

[S-TT38] Creating future of solid Earth science with high performance computing (HPC)

Sat. Jun 5, 2021 9:00 AM - 10:30 AM Ch.21 (Zoom Room 21)

convener:Takane Hori(R&D Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology), Yuji Yagi(Graduate School of Life and Environmental Sciences, University of Tsukuba, Tsukuba), Katsuhiko Shiomi(National Research Institute for Earth Science and Disaster Resilience), Ryoichiro Agata(Japan Agency for Marine-Earth Science and Technology), Chairperson:Takane Hori(R&D Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology), Ryoichiro Agata(Japan Agency for Marine-Earth Science and Technology)

10:00 AM - 10:15 AM

[STT38-05] Sensitivity analysis with large-scale 3D finite element crust structure model for seafloor geodetic constraints on coseismic slip and interseismic slip-deficit distributions

*Sota Murakami1, Tsuyoshi Ichimura1, Kohei Fujita1, Takane Hori2, Yusaku Ohta3 (1.Earthquake Research Institute, The University of Tokyo, 2.R&D Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology, 3.Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University)

Keywords:seafloor observation, inversion of fault slip, sensitivity analysis, crustal deformation, finite element analysis

Estimating the coseismic slip distribution and interseismic slip-deficit distribution play an important role in understanding the mechanism of massive earthquakes and predicting the resulting damage. It is useful to observe the crustal deformation not only in the land area, but also directly above the seismogenic zone. Therefore, improvements in terms of measurement precision and increase in the number of observation points have been proposed in various forms of seafloor observation. However, there is a room for developing a quantitative evaluation method of the estimation accuracy in cases where new crustal deformation observation points are available or when the precision of the observation methods have been improved. In this study, we proposed a method for quantitatively evaluating the improvement in the estimation accuracy of the coseismic slip distribution and the interseismic slip-deficit distribution in cases where new crustal deformation observation points are available or where the precision of the observation methods have been improved. We will present application examples based on large-scale finite element analysis using high-fidelity 3D crust structure and show the usefulness of the proposed method.