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DTSTAMP:20190719T085754Z
LOCATION:HG E 1.2
DTSTART;TZID=Europe/Stockholm:20190613T111500
DTEND;TZID=Europe/Stockholm:20190613T131500
UID:submissions.pasc-conference.org_PASC19_sess143@linklings.com
SUMMARY:MS16 - Advances in Computational Seismology and Earth Sciences, Pa
 rt I of III
DESCRIPTION:Minisymposium\nSolid Earth Dynamics\n\nExaHyPE: Towards Earthq
 uake Simulation Without Mesh Generation\n\nRannabauer, Duru, Gabriel, Bade
 r\n\nExaHyPE (www.exahype.eu) is a Horizon 2020 EU project to develop a hi
 gh-performance engine to solve hyperbolic systems of PDEs using the high-o
 rder discontinuous Galerkin finite element method. The project's goals are
  to develop an engine with flexible support for various applications which
  shall be...\n\n---------------------\nCoupled Multi-Physics Earthquake Sc
 enarios: from Long-Term Tectonics to Rupture Dynamics to Tsunami Simulatio
 ns\n\nGabriel, Ulrich, Madden, Duru, Uphoff\n\nEarthquakes are highly non-
 linear multiscale problems, encapsulating the geometry and rheology of pro
 pagating shear fractures that render the Earth’s crust and emanate d
 estructive seismic waves. Using physics-based earthquake scenarios, modern
  numerical methods and hardware specific optimizati...\n\n----------------
 -----\nUrgent Supercomputing for Earthquake Hazard Assessment\n\nde la Pue
 nte, Monterrubio\n\nEarthquakes can cause devastating effects and result i
 n terrible losses, both human and economical. Simulating their effects wit
 h 3D software is common practice. By modelling scenarios we can either stu
 dy past events or forecast the impact of hypothetical ones. Nevertheless, 
 the setup is time consum...\n\n---------------------\nMonitoring and Forec
 asting Methods for Crustal Activity in Subduction Zones with 3D Heterogene
 ous Medium using Large-Scale High-Fidelity Finite Element Simulations\n\nH
 ori, Ichimura, Fujita, Yamaguchi, Agata...\n\nTo analyze crustal activity 
 in the Earth's interior, such as spatio-temporal variation in slip velocit
 y on the plate interface including ordinary and slow earthquakes, we need 
 to use the data observed mostly on the Earth's surface. It is becoming int
 rinsic to consider 3D heterogeneous structure of t...\n
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