Articles | Volume 12, issue 6
https://doi.org/10.5194/tc-12-1969-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-12-1969-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
12 Jun 2018
Research article |
| 12 Jun 2018
Antarctic sub-shelf melt rates via PICO
Ronja Reese
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
University of Potsdam, Institute of Physics and Astronomy, Karl-Liebknecht-Str. 24-25, 14476 Potsdam, Germany
Torsten Albrecht
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
Matthias Mengel
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
Xylar Asay-Davis
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
Los Alamos National Laboratory, P.O. Box 1663, T-3, MS-B216, Los Alamos, NM 87545, USA
Ricarda Winkelmann
CORRESPONDING AUTHOR
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
University of Potsdam, Institute of Physics and Astronomy, Karl-Liebknecht-Str. 24-25, 14476 Potsdam, Germany
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- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al. 10.5194/tc-17-3203-2023
- A thicker Antarctic ice stream during the mid-Pliocene warm period M. Mas e Braga et al. 10.1038/s43247-023-00983-3
- Exploring risks and benefits of overshooting a 1.5 °C carbon budget over space and time N. Bauer et al. 10.1088/1748-9326/accd83
5 citations as recorded by crossref.
- Developments in Simulating and Parameterizing Interactions Between the Southern Ocean and the Antarctic Ice Sheet X. Asay-Davis et al. 10.1007/s40641-017-0071-0
- Extensive retreat and re-advance of the West Antarctic Ice Sheet during the Holocene J. Kingslake et al. 10.1038/s41586-018-0208-x
- Modelling present-day basal melt rates for Antarctic ice shelves using a parametrization of buoyant meltwater plumes W. Lazeroms et al. 10.5194/tc-12-49-2018
- Meeting User Needs for Sea Level Rise Information: A Decision Analysis Perspective J. Hinkel et al. 10.1029/2018EF001071
- The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing I. Tabone et al. 10.5194/cp-14-455-2018
Discussed (final revised paper)
Latest update: 19 Apr 2024
Short summary
Floating ice shelves surround most of Antarctica and ocean-driven melting at their bases is a major reason for its current sea-level contribution. We developed a simple model based on a box model approach that captures the vertical ocean circulation generally present in ice-shelf cavities and allows simulating melt rates in accordance with physical processes beneath the ice. We test the model for all Antarctic ice shelves and find that melt rates and melt patterns agree well with observations.
Floating ice shelves surround most of Antarctica and ocean-driven melting at their bases is a...
