Articles | Volume 13, issue 9
https://doi.org/10.5194/tc-13-2281-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-2281-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Sep 2019
Research article |
| 05 Sep 2019
| 05 Sep 2019
Modeling the response of Greenland outlet glaciers to global warming using a coupled flow line–plume model
Climate Impact Research (PIK), Member of the Leibniz Association,
P.O. Box 60 12 03,
14412 Potsdam, Germany
Mahé Perrette
Climate Impact Research (PIK), Member of the Leibniz Association,
P.O. Box 60 12 03,
14412 Potsdam, Germany
Sebastian Beyer
Climate Impact Research (PIK), Member of the Leibniz Association,
P.O. Box 60 12 03,
14412 Potsdam, Germany
Alfred Wegener Institute, 27570 Bremerhaven, Germany
Reinhard Calov
Climate Impact Research (PIK), Member of the Leibniz Association,
P.O. Box 60 12 03,
14412 Potsdam, Germany
Matteo Willeit
Climate Impact Research (PIK), Member of the Leibniz Association,
P.O. Box 60 12 03,
14412 Potsdam, Germany
Andrey Ganopolski
Climate Impact Research (PIK), Member of the Leibniz Association,
P.O. Box 60 12 03,
14412 Potsdam, Germany
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17 citations as recorded by crossref.
- Timescales of outlet-glacier flow with negligible basal friction: theory, observations and modeling J. Feldmann & A. Levermann 10.5194/tc-17-327-2023
- Modelled dynamic retreat of Kangerlussuaq Glacier, East Greenland, strongly influenced by the consecutive absence of an ice mélange in Kangerlussuaq Fjord J. Barnett et al. 10.1017/jog.2022.70
- Automated detection and characterization of Antarctic basal units using radar sounding data: demonstration in Institute Ice Stream, West Antarctica M. Goldberg et al. 10.1017/aog.2020.27
- Ice geometry and thermal regime of Lyngmarksbræen Ice Cap, West Greenland M. Gillespie et al. 10.1017/jog.2023.89
- Extensive inland thinning and speed-up of Northeast Greenland Ice Stream S. Khan et al. 10.1038/s41586-022-05301-z
- Effects of extreme melt events on ice flow and sea level rise of the Greenland Ice Sheet J. Beckmann & R. Winkelmann 10.5194/tc-17-3083-2023
- Twenty-first century ocean forcing of the Greenland ice sheet for modelling of sea level contribution D. Slater et al. 10.5194/tc-14-985-2020
- Greenland liquid water discharge from 1958 through 2019 K. Mankoff et al. 10.5194/essd-12-2811-2020
- Estimating Greenland tidewater glacier retreat driven by submarine melting D. Slater et al. 10.5194/tc-13-2489-2019
- A first constraint on basal melt-water production of the Greenland ice sheet N. Karlsson et al. 10.1038/s41467-021-23739-z
- Submarine Meltwater From Nioghalvfjerdsbræ (79 North Glacier), Northeast Greenland O. Huhn et al. 10.1029/2021JC017224
- Progress toward globally complete frontal ablation estimates of marine-terminating glaciers W. Kochtitzky et al. 10.1017/aog.2023.35
- Co-seismic eruption and intermittent turbulence of a subglacial discharge plume revealed by continuous subsurface observations in Greenland E. Podolskiy et al. 10.1038/s43247-021-00132-8
- Glacier–plume or glacier–fjord circulation models? A 2-D comparison for Hansbreen–Hansbukta system, Svalbard E. De Andrés et al. 10.1017/jog.2021.27
- The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6 H. Goelzer et al. 10.5194/tc-14-3071-2020
- Dynamic ice loss from the Greenland Ice Sheet driven by sustained glacier retreat M. King et al. 10.1038/s43247-020-0001-2
- Simulation of the future sea level contribution of Greenland with a new glacial system model R. Calov et al. 10.5194/tc-12-3097-2018
16 citations as recorded by crossref.
- Timescales of outlet-glacier flow with negligible basal friction: theory, observations and modeling J. Feldmann & A. Levermann 10.5194/tc-17-327-2023
- Modelled dynamic retreat of Kangerlussuaq Glacier, East Greenland, strongly influenced by the consecutive absence of an ice mélange in Kangerlussuaq Fjord J. Barnett et al. 10.1017/jog.2022.70
- Automated detection and characterization of Antarctic basal units using radar sounding data: demonstration in Institute Ice Stream, West Antarctica M. Goldberg et al. 10.1017/aog.2020.27
- Ice geometry and thermal regime of Lyngmarksbræen Ice Cap, West Greenland M. Gillespie et al. 10.1017/jog.2023.89
- Extensive inland thinning and speed-up of Northeast Greenland Ice Stream S. Khan et al. 10.1038/s41586-022-05301-z
- Effects of extreme melt events on ice flow and sea level rise of the Greenland Ice Sheet J. Beckmann & R. Winkelmann 10.5194/tc-17-3083-2023
- Twenty-first century ocean forcing of the Greenland ice sheet for modelling of sea level contribution D. Slater et al. 10.5194/tc-14-985-2020
- Greenland liquid water discharge from 1958 through 2019 K. Mankoff et al. 10.5194/essd-12-2811-2020
- Estimating Greenland tidewater glacier retreat driven by submarine melting D. Slater et al. 10.5194/tc-13-2489-2019
- A first constraint on basal melt-water production of the Greenland ice sheet N. Karlsson et al. 10.1038/s41467-021-23739-z
- Submarine Meltwater From Nioghalvfjerdsbræ (79 North Glacier), Northeast Greenland O. Huhn et al. 10.1029/2021JC017224
- Progress toward globally complete frontal ablation estimates of marine-terminating glaciers W. Kochtitzky et al. 10.1017/aog.2023.35
- Co-seismic eruption and intermittent turbulence of a subglacial discharge plume revealed by continuous subsurface observations in Greenland E. Podolskiy et al. 10.1038/s43247-021-00132-8
- Glacier–plume or glacier–fjord circulation models? A 2-D comparison for Hansbreen–Hansbukta system, Svalbard E. De Andrés et al. 10.1017/jog.2021.27
- The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6 H. Goelzer et al. 10.5194/tc-14-3071-2020
- Dynamic ice loss from the Greenland Ice Sheet driven by sustained glacier retreat M. King et al. 10.1038/s43247-020-0001-2
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
Submarine melting (SM) has been discussed as potentially triggering the recently observed retreat at outlet glaciers in Greenland. How much it may contribute in terms of future sea level rise (SLR) has not been quantified yet. When accounting for SM in our experiments, SLR contribution of 12 outlet glaciers increases by over 3-fold until the year 2100 under RCP8.5. Scaling up from 12 to all of Greenland's outlet glaciers increases future SLR contribution of Greenland by 50 %.
Submarine melting (SM) has been discussed as potentially triggering the recently observed...
