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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 6
The Cryosphere, 10, 3071–3089, 2016
https://doi.org/10.5194/tc-10-3071-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: International Partnerships in Ice Core Sciences (IPICS) Second...

The Cryosphere, 10, 3071–3089, 2016
https://doi.org/10.5194/tc-10-3071-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Dec 2016

Research article | 21 Dec 2016

Strain localization and dynamic recrystallization in the ice–air aggregate: a numerical study

Florian Steinbach et al.

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Cited articles

Alley, R. B.: Texture of polar firn for remote sensing, Ann. Glaciol., 9, 1–4, 1987.
Alley, R. B., Gow, A. J., and Meese, D. A.: Mapping c-axis fabrics to study physical processes in ice, J. Glaciol., 41, 197–203, 1995.
Anderson, D. L. and Benson, C. S.: The densification and diagenesis of snow, in: Ice and Snow: Properties, Processes and Applications, MIT Press, 1963.
Arena, L., Nasello, O. B., and Levi, L.: Effect of bubbles on grain growth in ice, J. Phys. Chem. B, 101, 6109–6112, 1997.
Azuma, N. and Higashi, A.: Formation processes of ice fabric pattern in ice sheets, Ann. Glaciol., 6, 130–134, 1985.
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Short summary
How glaciers or ice sheets flow is a result of microscopic processes controlled by the properties of individual ice crystals. We performed computer simulations on these processes and the effect of air bubbles between crystals. The simulations show that small-scale ice deformation is locally stronger than in other regions, which is enhanced by bubbles. This causes the ice crystals to recrystallise and change their properties in a way that potentially also affects the large-scale flow properties.
How glaciers or ice sheets flow is a result of microscopic processes controlled by the...
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