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The Cryosphere An interactive open-access journal of the European Geosciences Union
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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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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR by Anna Mirena Feist-Polner on behalf of the Authors (26 Jul 2017)  Author's response
ED: Publish subject to technical corrections (21 Aug 2017) by Olivier Gagliardini
Publications Copernicus
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Short summary
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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