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Volume 11, issue 5
The Cryosphere, 11, 2283–2303, 2017
https://doi.org/10.5194/tc-11-2283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 11, 2283–2303, 2017
https://doi.org/10.5194/tc-11-2283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 05 Oct 2017

Research article | 05 Oct 2017

Boundary layer models for calving marine outlet glaciers

Christian Schoof et al.

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Cited articles

Bassis, J. and Jacobs, S.: Diverse calving patterns linked to glacier geometry, Nat. Geosci., 6, 833–836, https://doi.org/10.1038/NGEO1887, 2013.
Bassis, J. and Walker, C.: Upper and lower limits on the stability of calving glaciers from the yield strength envelope of ice, P. R. Soc. Lond. A, 468, 913–931, 2011.
Budd, W., Keage, P., and Blundy, N.: Empirical studies of ice sliding, J. Glaciol., 23, 157–170, 1979.
Dupont, T. and Alley, R.: Assessment of the importance of ice-shelf buttressing to ice sheet flows, Geophys. Res. Lett., 32, L04503, https://doi.org/10.1029/2004GL022024, 2005.
Fowler, A.: A theoretical treatment of the sliding of glaciers in the absence of cavitation, Philos. T. R. Soc. Lond., 298, 637–685, 1981.
Publications Copernicus
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We show mathematically and computationally how discharge of ice from ocean-terminating glaciers is controlled by a combination of different forces acting on ice near the grounding line of a glacier and how that combination of forces is affected by the process of iceberg formation, which limits the length of floating ice tongues extending in front of the glacier. We show that a deeper fjord may lead to a longer ice tongue providing greater drag on the glacier, slowing the rate of ice discharge.
We show mathematically and computationally how discharge of ice from ocean-terminating glaciers...
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