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Published on: January 6, 2023
A Generalized Interpolation Material Point Method for Shallow Ice Shelves. 1: Shallow Shelf Approximation and Ice
Alex Huth1,2, Ravindra Duddu3,4, Ben Smith5
1Department of Earth and Space Sciences University of Washington Seattle WA USA.
We developed a new numerical method, the generalized interpolation material point method (GIMPM), to accurately simulate ice flow dynamics. This GIMPM-SSA framework overcomes limitations of previous methods, enabling precise tracking of ice shelves and grounding lines.
Area of Science:
- Glaciology and Computational Fluid Dynamics
- Numerical methods for geophysical flows
- Ice sheet and ice shelf dynamics modeling
Background:
- Accurate simulation of ice flow is crucial for understanding climate change impacts.
- Existing methods like the standard material point method (sMPM) suffer from significant grid-crossing errors in shallow shelf approximation (SSA) simulations.
- Tracking ice fronts and grounding lines at high resolution remains a challenge.
Purpose of the Study:
- To develop and validate a novel numerical framework, the generalized interpolation material point method (GIMPM), for simulating ice flow under the shallow shelf approximation (SSA).
- To address limitations of existing methods, particularly grid-crossing errors and difficulties in boundary tracking.
- To enable efficient and accurate advection of state variables without diffusion errors.
Main Methods:
- Implementation of the GIMPM, a particle-based method analogous to the finite element method, for solving SSA equations.
- Development of novel numerical schemes for particle splitting and integration at domain boundaries.
- Comparison of GIMPM-SSA with the standard material point method (sMPM) and a reweighted sMPM using 1-D and 2-D benchmark cases.
Main Results:
- The GIMPM successfully mitigates severe grid-crossing errors inherent in sMPM simulations of SSA.
- The GIMPM demonstrates superior accuracy compared to reweighted sMPM approaches.
- Automated tracking of ice fronts and grounding lines at sub-element scales is achieved.
- Efficient advection of history or internal state variables (e.g., ice thickness, damage) without diffusion errors is confirmed.
Conclusions:
- The GIMPM-SSA framework is a viable and accurate tool for simulating ice sheet-shelf evolution.
- This method offers significant advantages in boundary tracking and error-free advection of state variables.
- The GIMPM represents a substantial advancement for high-fidelity ice flow modeling.
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