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Full Stokes modeling of marine ice sheets: influence of the grid size

Abstract : Using the finite-element code Elmer, we show that the full Stokes modeling of the ice-sheet/ice-shelf transition we propose can give consistent predictions of grounding-line migration. Like other marine ice-sheet models our approach is highly sensitive to the chosen mesh resolution. However, with a grid size down to <5 km in the vicinity of the grounding line, predictions start to be robust because: (1) whatever the grid size (<5 km) the steady-state grounding-line position is sensibly the same (6 km standard deviation), and (2) with a grid-size refinement in the vicinity of the grounding line (200 m), the steady-state solution is independent of the applied perturbation in fluidity, provided this perturbation remains monotonic.
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Contributor : Aurore Gayraud <>
Submitted on : Tuesday, September 29, 2009 - 4:08:10 PM
Last modification on : Tuesday, December 8, 2020 - 10:49:05 AM

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Gaël Durand, Olivier Gagliardini, Thomas Zwinger, Emmanuel Le Meur, Richard C.A. Hindmarsh. Full Stokes modeling of marine ice sheets: influence of the grid size. Annals of Glaciology, International Glaciological Society, 2009, 50 (52), pp.109-114(6). ⟨10.3189/172756409789624283⟩. ⟨insu-00420761⟩



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