Benchmarking the vertically integrated ice-sheet model IMAU-ICE (version 2.0)

<p>Ice-dynamical processes constitute a large uncertainty in future projections of sea-level rise caused by anthropogenic climate change. Improving our understanding of these processes requires ice-sheet models that perform well at simulating both past and future ice-sheet evolution. Here, we...

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Bibliographic Details
Main Authors: C. J. Berends, H. Goelzer, T. J. Reerink, L. B. Stap, R. S. W. van de Wal
Format: Article
Language:English
Published: Copernicus Publications 2022-07-01
Series:Geoscientific Model Development
Online Access:https://gmd.copernicus.org/articles/15/5667/2022/gmd-15-5667-2022.pdf
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Summary:<p>Ice-dynamical processes constitute a large uncertainty in future projections of sea-level rise caused by anthropogenic climate change. Improving our understanding of these processes requires ice-sheet models that perform well at simulating both past and future ice-sheet evolution. Here, we present version 2.0 of the ice-sheet model IMAU-ICE, which uses the depth-integrated viscosity approximation (DIVA) to solve the stress balance. We evaluate its performance in a range of benchmark experiments, including simple analytical solutions and both schematic and realistic model intercomparison exercises. IMAU-ICE has adopted recent developments in the numerical treatment of englacial stress and sub-shelf melt near the grounding line, which result in good performance in experiments concerning grounding-line migration (MISMIP, MISMIP<span class="inline-formula">+)</span> and buttressing (ABUMIP). This makes it a model that is robust, versatile, and user-friendly, which will provide a firm basis for (palaeo-)glaciological research in the coming years.</p>
ISSN:1991-959X
1991-9603