Abstract
This article comments on some basic glaciological algorithms for solving the shallow-ice-approximation-based ice-sheet equation and the motion of tracers within ice. The emphasis is practical, with discussion of the merits and demerits of popular algorithms.
Finite difference, pseudo-spectral and characteristic methods are compared for the tracer equation. Second-order upstreaming is found to give the most robust results.
Robust stability criteria applicable to explicit and semi-implicit marching schemes for the ice-sheet equation are derived. The accuracies of three spatial discretization methods are compared; one method is clearly more accurate than the others, but requires twice as much computation time per time-step. A stable semi-implicit method for the ice-sheet equation is suggested by the stability analyses in this paper.
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Hindmarsh, R.C.A. (2001). Notes on Basic Glaciological Computational Methods and Algorithms. In: Straughan, B., Greve, R., Ehrentraut, H., Wang, Y. (eds) Continuum Mechanics and Applications in Geophysics and the Environment. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-04439-1_13
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DOI: https://doi.org/10.1007/978-3-662-04439-1_13
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