Abstract
Many problems in geodynamic modelling result in a non-linear Stokes problem in which the viscosity depends on the strain rate and pressure (in addition to other variables). After discretization, the resulting non-linear system is most commonly solved using a Picard fixedpoint iteration. However, it is well understood that Newton's method - when augmented by globalization strategies to ensure convergence even from points far from the solution - can be substantially more efficient and accurate than a Picard solver. In this contribution, we evaluate how a straightforward Newton method must be modified to allow for the kinds of rheologies common in geodynamics. Specifically, we show that the Newton step is not actually well posed for strain rate-weakening models without modifications to the Newton matrix. We derive modifications that guarantee well posedness and that also allow for efficient solution strategies by ensuring that the top left block of the Newton matrix is symmetric and positive definite.We demonstrate the applicability and relevance of thesemodifications with a sequence of benchmarks and a test case of realistic complexity.
Original language | English |
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Pages (from-to) | 873-894 |
Number of pages | 22 |
Journal | Geophysical Journal International |
Volume | 218 |
Issue number | 2 |
DOIs | |
Publication status | Published - Aug 2019 |
Funding
This work is funded by the Netherlands Organization for Scientific Research (NWO), as part of the Caribbean Research program, grant number 858.14.070, as well as by the NWO project ‘Large scale finite element models of the Caribbean region: Newton versus Picard non-linear iterations’ with project number 15820. We acknowledge computational support by theNetherlands Research Centre for Integrated Solid Earth Science (ISES). WB’s work was partially supported by the Computational Infrastructure in Geodynamics initiative (CIG), through the National Science Foundation under award number EAR-0949446 and The University of California – Davis; and by the National Science Foundation under awards OCI-1148116 and OAC-1835673 as part of the Software Infrastructure for Sustained Innovation (SI2) program (now the Cyberinfrastructure for Sustained Scientific Innovation, CSSI). WS acknowledges support from the Research Council of Norway through its Centres of Excellence funding scheme, project number 223272.
Keywords
- Dynamics and mechanics of faulting
- Dynamics of lithosphere and mantle
- Non-linear differential equations
- Numerical modeling
- Subduction zone processes.