Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
The Cryosphere, 11, 319-329, 2017
http://www.the-cryosphere.net/11/319/2017/
doi:10.5194/tc-11-319-2017
© Author(s) 2017. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
31 Jan 2017
Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting
Rupert Michael Gladstone1,2,3, Roland Charles Warner2, Benjamin Keith Galton-Fenzi2,4, Olivier Gagliardini5, Thomas Zwinger6, and Ralf Greve7 1VAW, Eidgenössische Technische Hochschule Zürich, ETHZ, Zürich, Switzerland
2Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Australia
3Arctic Centre, University of Lapland, Rovaniemi, Finland
4Australian Antarctic Division, Kingston, Tasmania, Australia
5Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
6CSC – IT Center for Science Ltd., Espoo, Finland
7Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan
Abstract. Computer models are necessary for understanding and predicting marine ice sheet behaviour. However, there is uncertainty over implementation of physical processes at the ice base, both for grounded and floating glacial ice. Here we implement several sliding relations in a marine ice sheet flow-line model accounting for all stress components and demonstrate that model resolution requirements are strongly dependent on both the choice of basal sliding relation and the spatial distribution of ice shelf basal melting.

Sliding relations that reduce the magnitude of the step change in basal drag from grounded ice to floating ice (where basal drag is set to zero) show reduced dependence on resolution compared to a commonly used relation, in which basal drag is purely a power law function of basal ice velocity. Sliding relations in which basal drag goes smoothly to zero as the grounding line is approached from inland (due to a physically motivated incorporation of effective pressure at the bed) provide further reduction in resolution dependence.

A similar issue is found with the imposition of basal melt under the floating part of the ice shelf: melt parameterisations that reduce the abruptness of change in basal melting from grounded ice (where basal melt is set to zero) to floating ice provide improved convergence with resolution compared to parameterisations in which high melt occurs adjacent to the grounding line.

Thus physical processes, such as sub-glacial outflow (which could cause high melt near the grounding line), impact on capability to simulate marine ice sheets. If there exists an abrupt change across the grounding line in either basal drag or basal melting, then high resolution will be required to solve the problem. However, the plausible combination of a physical dependency of basal drag on effective pressure, and the possibility of low ice shelf basal melt rates next to the grounding line, may mean that some marine ice sheet systems can be reliably simulated at a coarser resolution than currently thought necessary.


Citation: Gladstone, R. M., Warner, R. C., Galton-Fenzi, B. K., Gagliardini, O., Zwinger, T., and Greve, R.: Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting, The Cryosphere, 11, 319-329, doi:10.5194/tc-11-319-2017, 2017.
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Short summary
Computer models are used to simulate the behaviour of glaciers and ice sheets. It has been found that such models are required to be run at very high resolution (which means high computational expense) in order to accurately represent the evolution of marine ice sheets (ice sheets resting on bedrock below sea level), in certain situations which depend on sub-glacial physical processes.
Computer models are used to simulate the behaviour of glaciers and ice sheets. It has been found...
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