Japan Geoscience Union Meeting 2022

Presentation information

[J] Oral

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

[S-TT41] Creating future of solid Earth science with high performance computing (HPC)

Sun. May 22, 2022 9:00 AM - 10:30 AM 301A (International Conference Hall, Makuhari Messe)

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

9:00 AM - 9:15 AM

[STT41-01] Extremely Large-scale earthquake cycle simulations using lattice H-matrices

★Invited Papers

*So Ozawa1, Akihiro Ida2, Ryosuke Ando3, Tetsuya Hoshino1 (1.Graduate School of Science, the University of Tokyo, 2.Japan Agency for Marine-Earth Science and Technology, 3.Information Technology Center, the University of Tokyo)

Keywords:HPC, Boundary element method, Earthquake cycle Simulation

Large-scale earthquake sequence simulations using the boundary element method (BEM) incur extreme computational costs through multiplying a dense matrix with a slip rate vector. Recently, hierarchical matrices (H-matrices) have often been used to accelerate this multiplication. However, the complexity of the structures of the H-matrices and the communication costs between processors limit their scalability, and they therefore cannot be used efficiently in distributed memory computer systems. Lattice H-matrices have recently been proposed as a tool to improve the parallel scalability of H-matrices.

In this study, we develop a method for earthquake sequence simulations applicable to 3D nonplanar faults with lattice H-matrices. We present a simulation example and verify the accuracy of our method for a 3D nonplanar thrust fault. We also performed performance and scalability analyses of our code. Our simulations, using over 100,000 degrees of freedom, demonstrated a parallel acceleration beyond MPI processors and a >10-fold acceleration over the best performance when the normal H-matrices are used. Using this code, we can perform unprecedented large-scale earthquake sequence simulations on geometrically complex faults with supercomputers.