Articles | Volume 16, issue 2
https://doi.org/10.5194/tc-16-581-2022
© Author(s) 2022. 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-16-581-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
17 Feb 2022
Research article |
| 17 Feb 2022
| 17 Feb 2022
Geometric controls of tidewater glacier dynamics
Department of Earth Science, University of Bergen, Bjerknes Centre for Climate Research, Bergen, Norway
Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Henning Åkesson
Department of Geological Sciences, Stockholm University, Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm, Sweden
Department of Geosciences, University of Oslo, Oslo, Norway
Basile de Fleurian
Department of Earth Science, University of Bergen, Bjerknes Centre for Climate Research, Bergen, Norway
Mathieu Morlighem
Department of Earth Sciences, Dartmouth College, Hanover, NH, USA
Department of Earth System Science, University of California, Irvine, CA, USA
Kerim H. Nisancioglu
Department of Earth Science, University of Bergen, Bjerknes Centre for Climate Research, Bergen, Norway
Centre for Earth Evolution and Dynamics, University of Oslo, Oslo, Norway
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Total article views: 1,949 (including HTML, PDF, and XML)
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Total article views: 1,138 (including HTML, PDF, and XML)
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Cited
12 citations as recorded by crossref.
- Ice volume and thickness of all Scandinavian glaciers and ice caps T. Frank & W. van Pelt 10.1017/jog.2024.25
- Effects of topography on dynamics and mass loss of lake-terminating glaciers in southern Patagonia M. Minowa et al. 10.1017/jog.2023.42
- Contextual HookFormer for Glacier Calving Front Segmentation F. Wu et al. 10.1109/TGRS.2024.3368215
- Projected sea-level contributions from tidewater glaciers are highly sensitive to chosen bedrock topography: a case study at Hansbreen, Svalbard M. Möller et al. 10.1017/jog.2022.117
- Combining “Deep Learning” and Physically Constrained Neural Networks to Derive Complex Glaciological Change Processes from Modern High-Resolution Satellite Imagery: Application of the GEOCLASS-Image System to Create VarioCNN for Glacier Surges U. Herzfeld et al. 10.3390/rs16111854
- Characteristics of dynamic thickness change across diverse outlet glacier geometries and basal conditions D. Yang et al. 10.1017/jog.2024.50
- AMD-HookNet for Glacier Front Segmentation F. Wu et al. 10.1109/TGRS.2023.3245419
- Capturing the transition from marine to land-terminating glacier from the 126-year retreat history of Nordenskiöldbreen, Svalbard J. Kavan et al. 10.1017/jog.2023.92
- Iceberg Calving: Regimes and Transitions R. Alley et al. 10.1146/annurev-earth-032320-110916
- Widespread seasonal speed-up of west Antarctic Peninsula glaciers from 2014 to 2021 B. Wallis et al. 10.1038/s41561-023-01131-4
- Nunataks as barriers to ice flow: implications for palaeo ice sheet reconstructions M. Mas e Braga et al. 10.5194/tc-15-4929-2021
- Helheim Glacier Poised for Dramatic Retreat J. Williams et al. 10.1029/2021GL094546
10 citations as recorded by crossref.
- Ice volume and thickness of all Scandinavian glaciers and ice caps T. Frank & W. van Pelt 10.1017/jog.2024.25
- Effects of topography on dynamics and mass loss of lake-terminating glaciers in southern Patagonia M. Minowa et al. 10.1017/jog.2023.42
- Contextual HookFormer for Glacier Calving Front Segmentation F. Wu et al. 10.1109/TGRS.2024.3368215
- Projected sea-level contributions from tidewater glaciers are highly sensitive to chosen bedrock topography: a case study at Hansbreen, Svalbard M. Möller et al. 10.1017/jog.2022.117
- Combining “Deep Learning” and Physically Constrained Neural Networks to Derive Complex Glaciological Change Processes from Modern High-Resolution Satellite Imagery: Application of the GEOCLASS-Image System to Create VarioCNN for Glacier Surges U. Herzfeld et al. 10.3390/rs16111854
- Characteristics of dynamic thickness change across diverse outlet glacier geometries and basal conditions D. Yang et al. 10.1017/jog.2024.50
- AMD-HookNet for Glacier Front Segmentation F. Wu et al. 10.1109/TGRS.2023.3245419
- Capturing the transition from marine to land-terminating glacier from the 126-year retreat history of Nordenskiöldbreen, Svalbard J. Kavan et al. 10.1017/jog.2023.92
- Iceberg Calving: Regimes and Transitions R. Alley et al. 10.1146/annurev-earth-032320-110916
- Widespread seasonal speed-up of west Antarctic Peninsula glaciers from 2014 to 2021 B. Wallis et al. 10.1038/s41561-023-01131-4
Latest update: 22 Nov 2024
Short summary
The shape of a fjord can promote or inhibit glacier retreat in response to climate change. We conduct experiments with a synthetic setup under idealized conditions in a numerical model to study and quantify the processes involved. We find that friction between ice and fjord is the most important factor and that it is possible to directly link ice discharge and grounding line retreat to fjord topography in a quantitative way.
The shape of a fjord can promote or inhibit glacier retreat in response to climate change. We...
