Status: this preprint is open for discussion and under review for Geoscientific Model Development (GMD).
A comparison of the accuracy and stability of numerical schemes used to solve the equations derived from the shallow-shelf approximation
Deborah Rhee,Sainan Sun,and G. Hilmar Gudmundsson
Abstract. The shallow-shelf approximation (SSA) is widely used to model the evolution of fast-flowing ice that is either floating or sliding rapidly over the bed, resulting in plug flow. However, so far there has been no rigorous, comparative study of the different numerical approaches to solve the SSA equations. We calculate the conditions for different numerical schemes to remain stable and accurate when solving the linear 1D SSA equations for a simple geometry. The comparison spans central difference and upwind schemes, explicit and semi-implicit multistep schemes, and explicit or implicit monolithic schemes. Also considered are schemes time stepping using the Θ-method, where the value of Θ is used to form a weighted combination of the forward and backward Euler methods. We find that monolithic schemes remain stable at all tested time steps for Θ ≥ 0.5 whilst multistep schemes become unstable at large time steps. Of the tested schemes the monolithic finite element scheme with Θ = 0.5 remains accurate for the largest range of time steps.
Received: 18 Aug 2026 – Discussion started: 12 Oct 2026
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Data and code for "A comparison of the accuracy and stability of numerical schemes used to solve the equations derived from the shallow-shelf approximation"Deborah Rhee https://doi.org/10.5281/zenodo.21977299
Model code and software
Data and code for "A comparison of the accuracy and stability of numerical schemes used to solve the equations derived from the shallow-shelf approximation"Deborah Rhee https://doi.org/10.5281/zenodo.21977299
Deborah Rhee,Sainan Sun,and G. Hilmar Gudmundsson
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The shallow-shelf approximation (SSA) is widely used to model the evolution of fast-flowing ice. Various numerical schemes are used to solve the equations resulting from the SSA. We find the range of parameters under which each scheme remains stable and accurate. The optimum tested scheme solves the equations simultaneously using the finite element method with Lax-Wendroff time stepping. Results in this manuscript inform the development of future models and parameter choices in current models.
The shallow-shelf approximation (SSA) is widely used to model the evolution of fast-flowing ice....