Journal
GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 227, Issue 1, Pages 632-643Publisher
OXFORD UNIV PRESS
DOI: 10.1093/gji/ggab237
Keywords
Time variable gravity; Numerical modelling; Computational seismology; Surface waves and free oscillations
Categories
Funding
- Swiss National Supercomputing Centre (CSCS) [s922]
- European Research Council (ERC) under the EU [714069]
- Swiss National Science Foundation [172508, 197369]
- European Research Council (ERC) [714069] Funding Source: European Research Council (ERC)
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A new approach is presented for solving the Poisson equation in the global seismic wave propagation in time domain, aiming to include the full gravitational response in spectral element solvers. By leveraging adaptive mesh refinement and high order shape mapping using Salvus meshing software, the number of additional elements needed is minimized. Initial conditions based on temporal extrapolation and a polynomial multigrid method reduce the number of iterations needed for convergence.
We present a new approach to the solution of the Poisson equation present in the coupled gravito-elastic equations of motion for global seismic wave propagation in time domain aiming at the inclusion of the full gravitational response into spectral element solvers. We leverage the Salvus meshing software to include the external domain using adaptive mesh refinement and high order shape mapping. Together with Neumann boundary conditions based on a multipole expansion of the right-hand side this minimizes the number of additional elements needed. Initial conditions for the iterative solution of the Poisson equation based on temporal extrapolation from previous time steps together with a polynomialmultigridmethod reduce the number of iterations needed for convergence. In summary, this approach reduces the extra cost for simulating full gravity to a similar order as the elastic forces. We demonstrate the efficacy of the proposed method using the displacement from an elastic global wave propagation simulation (decoupled from the Poisson equation) at 200 s dominant period to compute a realistic right-hand side for the Poisson equation.
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