Articles | Volume 14, issue 4
https://doi.org/10.5194/tc-14-1245-2020
© Author(s) 2020. 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-14-1245-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Apr 2020
Research article |
| 15 Apr 2020
| 15 Apr 2020
Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100
Alanna V. Alevropoulos-Borrill
CORRESPONDING AUTHOR
Centre for Polar Observation and Modelling, School of Geographical
Sciences, University of Bristol, University Road, Bristol, BS8 1SS, UK
now at: Antarctic Research Centre, Victoria University of Wellington, Wellington, 6012, New Zealand
Isabel J. Nias
Centre for Polar Observation and Modelling, School of Geographical
Sciences, University of Bristol, University Road, Bristol, BS8 1SS, UK
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
Antony J. Payne
Centre for Polar Observation and Modelling, School of Geographical
Sciences, University of Bristol, University Road, Bristol, BS8 1SS, UK
Nicholas R. Golledge
Antarctic Research Centre, Victoria University of Wellington,
Wellington, 6012, New Zealand
Rory J. Bingham
Centre for Polar Observation and Modelling, School of Geographical
Sciences, University of Bristol, University Road, Bristol, BS8 1SS, UK
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Cited
14 citations as recorded by crossref.
- Strong Ocean Melting Feedback During the Recent Retreat of Thwaites Glacier P. Holland et al. 10.1029/2023GL103088
- Projected land ice contributions to twenty-first-century sea level rise T. Edwards et al. 10.1038/s41586-021-03302-y
- Quantifying the Impact of Bedrock Topography Uncertainty in Pine Island Glacier Projections for This Century A. Wernecke et al. 10.1029/2021GL096589
- Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica J. Johnson et al. 10.1029/2020JF005827
- Melt sensitivity of irreversible retreat of Pine Island Glacier B. Reed et al. 10.5194/tc-18-4567-2024
- Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change S. Bevan et al. 10.1017/jog.2023.57
- Probabilistic projections of the Amery Ice Shelf catchment, Antarctica, under conditions of high ice-shelf basal melt S. Jantre et al. 10.5194/tc-18-5207-2024
- Coupled ice–ocean interactions during future retreat of West Antarctic ice streams in the Amundsen Sea sector D. Bett et al. 10.5194/tc-18-2653-2024
- Derivation of bedrock topography measurement requirements for the reduction of uncertainty in ice-sheet model projections of Thwaites Glacier B. Castleman et al. 10.5194/tc-16-761-2022
- Quantifying the potential future contribution to global mean sea level from the Filchner–Ronne basin, Antarctica E. Hill et al. 10.5194/tc-15-4675-2021
- The influence of emissions scenarios on future Antarctic ice loss is unlikely to emerge this century D. Lowry et al. 10.1038/s43247-021-00289-2
- Sustained ocean cooling insufficient to reverse sea level rise from Antarctica A. Alevropoulos-Borrill et al. 10.1038/s43247-024-01297-8
- The transferability of adjoint inversion products between different ice flow models J. Barnes et al. 10.5194/tc-15-1975-2021
- Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100 A. Alevropoulos-Borrill et al. 10.5194/tc-14-1245-2020
13 citations as recorded by crossref.
- Strong Ocean Melting Feedback During the Recent Retreat of Thwaites Glacier P. Holland et al. 10.1029/2023GL103088
- Projected land ice contributions to twenty-first-century sea level rise T. Edwards et al. 10.1038/s41586-021-03302-y
- Quantifying the Impact of Bedrock Topography Uncertainty in Pine Island Glacier Projections for This Century A. Wernecke et al. 10.1029/2021GL096589
- Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica J. Johnson et al. 10.1029/2020JF005827
- Melt sensitivity of irreversible retreat of Pine Island Glacier B. Reed et al. 10.5194/tc-18-4567-2024
- Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change S. Bevan et al. 10.1017/jog.2023.57
- Probabilistic projections of the Amery Ice Shelf catchment, Antarctica, under conditions of high ice-shelf basal melt S. Jantre et al. 10.5194/tc-18-5207-2024
- Coupled ice–ocean interactions during future retreat of West Antarctic ice streams in the Amundsen Sea sector D. Bett et al. 10.5194/tc-18-2653-2024
- Derivation of bedrock topography measurement requirements for the reduction of uncertainty in ice-sheet model projections of Thwaites Glacier B. Castleman et al. 10.5194/tc-16-761-2022
- Quantifying the potential future contribution to global mean sea level from the Filchner–Ronne basin, Antarctica E. Hill et al. 10.5194/tc-15-4675-2021
- The influence of emissions scenarios on future Antarctic ice loss is unlikely to emerge this century D. Lowry et al. 10.1038/s43247-021-00289-2
- Sustained ocean cooling insufficient to reverse sea level rise from Antarctica A. Alevropoulos-Borrill et al. 10.1038/s43247-024-01297-8
- The transferability of adjoint inversion products between different ice flow models J. Barnes et al. 10.5194/tc-15-1975-2021
1 citations as recorded by crossref.
Latest update: 21 Feb 2025
