the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A Fully Implicit Second Order Method for Viscous Free Surface Stokes Flow – Application to Glacier Simulations
Abstract. We present a fully implicit finite element method for viscous free surface Stokes problems which are common in glaciology and geodynamics. Standard fully implicit iterative solvers diverge for such problems when using large time steps. We address this by incorporating a stabilization term that vanishes upon convergence. This approach enables the use of large time steps, thereby significantly improving the efficiency of simulations. Furthermore, we leverage the fully implicit solver to develop second-order time-stepping schemes that mitigate the high errors associated with first-order methods for large time steps. The methods are tested and evaluated on model domains relevant to geodynamics and glaciology.
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Status: open (until 26 Nov 2025)
- CEC1: 'No compliance with the policy of the journal', Juan Antonio Añel, 07 Oct 2025 reply
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Dear authors,
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Juan A. Añel
Geosci. Model Dev. Executive Editor