1University of Texas Institute for Geophysics, J.J. Pickle Research
Campus, Building 196, 10100 Burnet Road (R2200), Austin, TX 78758-4445, USA
2Jet Propulsion Laboratory – California Institute of technology, 4800
Oak Grove Drive MS 300-323, Pasadena, CA 91109-8099, USA
of California, Irvine, Department of Earth System Science, Croul Hall, Irvine,
CA 92697-3100, USA
4Department of Arctic Geophysics, University Centre
in Svalbard, Longyearbyen, Norway
Received: 04 May 2016 – Discussion started: 17 May 2016
Abstract. Identifying fast and robust numerical solvers is a critical issue that needs to be addressed in order to improve projections of polar ice sheets evolving in a changing climate. This work evaluates the impact of using advanced numerical solvers for transient ice-flow simulations conducted with the JPL–UCI Ice Sheet System Model (ISSM). We identify optimal numerical solvers by testing a broad suite of readily available solvers, ranging from direct sparse solvers to preconditioned iterative methods, on the commonly used Ice Sheet Model Intercomparison Project for Higher-Order ice sheet Models benchmark tests. Three types of analyses are considered: mass transport, horizontal stress balance, and incompressibility. The results of the fastest solvers for each analysis type are ranked based on their scalability across mesh size and basal boundary conditions. We find that the fastest iterative solvers are ∼ 1.5–100 times faster than the default direct solver used in ISSM, with speed-ups improving rapidly with increased mesh resolution. We provide a set of recommendations for users in search of efficient solvers to use for transient ice-flow simulations, enabling higher-resolution meshes and faster turnaround time. The end result will be improved transient simulations for short-term, highly resolved forward projections (10–100 year time scale) and also improved long-term paleo-reconstructions using higher-order representations of stresses in the ice. This analysis will also enable a new generation of comprehensive uncertainty quantification assessments of forward sea-level rise projections, which rely heavily on ensemble or sampling approaches that are inherently expensive.
Revised: 17 Nov 2016 – Accepted: 24 Nov 2016 – Published: 10 Jan 2017
Habbal, F., Larour, E., Morlighem, M., Seroussi, H., Borstad, C. P., and Rignot, E.: Optimal numerical solvers for transient simulations of ice flow using the Ice Sheet System Model (ISSM versions 4.2.5 and 4.11), Geosci. Model Dev., 10, 155-168, doi:10.5194/gmd-10-155-2017, 2017.