Articles | Volume 16, issue 7
https://doi.org/10.5194/tc-16-2725-2022
© 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-16-2725-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats
John Erich Christian
CORRESPONDING AUTHOR
Institute for Geophysics, University of Texas at Austin, Austin, Texas 78758, USA
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30318, USA
Alexander A. Robel
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30318, USA
Ginny Catania
Institute for Geophysics, University of Texas at Austin, Austin, Texas 78758, USA
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Cited
16 citations as recorded by crossref.
- Characteristics of dynamic thickness change across diverse outlet glacier geometries and basal conditions D. Yang et al. 10.1017/jog.2024.50
- Climatology and surface impacts of atmospheric rivers on West Antarctica M. Maclennan et al. 10.5194/tc-17-865-2023
- ‘Stable’ and ‘unstable’ are not useful descriptions of marine ice sheets in the Earth's climate system O. Sergienko & M. Haseloff 10.1017/jog.2023.40
- A framework for estimating the anthropogenic part of Antarctica’s sea level contribution in a synthetic setting A. Bradley et al. 10.1038/s43247-024-01287-w
- Atlantic water intrusion triggers rapid retreat and regime change at previously stable Greenland glacier T. Chudley et al. 10.1038/s41467-023-37764-7
- Potential geographic displacement of Chagas disease vectors under climate change L. Brasil et al. 10.1111/mve.12810
- The Stochastic Ice-Sheet and Sea-Level System Model v1.0 (StISSM v1.0) V. Verjans et al. 10.5194/gmd-15-8269-2022
- Diverse behaviors of marine ice sheets in response to temporal variability of the atmospheric and basal conditions O. Sergienko & D. Wingham 10.1017/jog.2024.43
- Characteristics and rarity of the strong 1940s westerly wind event over the Amundsen Sea, West Antarctica G. O'Connor et al. 10.5194/tc-17-4399-2023
- Description and validation of the ice-sheet model Nix v1.0 D. Moreno-Parada et al. 10.5194/gmd-18-3895-2025
- Biases in ice sheet models from missing noise-induced drift A. Robel et al. 10.5194/tc-18-2613-2024
- Glacier damage evolution over ice flow timescales M. Ranganathan et al. 10.5194/tc-19-1599-2025
- Topographic modulation of outlet glaciers in Greenland: a review G. Catania & D. Felikson 10.1017/aog.2023.55
- Predicting glacial lake outburst susceptibility on the southern Tibetan Plateau with historical events and machine learning methods H. Liu et al. 10.1007/s11069-025-07486-8
- Exploring potential glacial lakes using geo-spatial techniques in Eastern Hindu Kush Region, Pakistan M. Sarwar & S. Mahmood 10.1016/j.nhres.2023.07.003
- The Hunga Tonga–Hunga Haʻapai volcanic barometric pressure pulse and meteotsunami travel recorded in several Antarctic stations H. EVANGELISTA et al. 10.1590/0001-3765202420240556
16 citations as recorded by crossref.
- Characteristics of dynamic thickness change across diverse outlet glacier geometries and basal conditions D. Yang et al. 10.1017/jog.2024.50
- Climatology and surface impacts of atmospheric rivers on West Antarctica M. Maclennan et al. 10.5194/tc-17-865-2023
- ‘Stable’ and ‘unstable’ are not useful descriptions of marine ice sheets in the Earth's climate system O. Sergienko & M. Haseloff 10.1017/jog.2023.40
- A framework for estimating the anthropogenic part of Antarctica’s sea level contribution in a synthetic setting A. Bradley et al. 10.1038/s43247-024-01287-w
- Atlantic water intrusion triggers rapid retreat and regime change at previously stable Greenland glacier T. Chudley et al. 10.1038/s41467-023-37764-7
- Potential geographic displacement of Chagas disease vectors under climate change L. Brasil et al. 10.1111/mve.12810
- The Stochastic Ice-Sheet and Sea-Level System Model v1.0 (StISSM v1.0) V. Verjans et al. 10.5194/gmd-15-8269-2022
- Diverse behaviors of marine ice sheets in response to temporal variability of the atmospheric and basal conditions O. Sergienko & D. Wingham 10.1017/jog.2024.43
- Characteristics and rarity of the strong 1940s westerly wind event over the Amundsen Sea, West Antarctica G. O'Connor et al. 10.5194/tc-17-4399-2023
- Description and validation of the ice-sheet model Nix v1.0 D. Moreno-Parada et al. 10.5194/gmd-18-3895-2025
- Biases in ice sheet models from missing noise-induced drift A. Robel et al. 10.5194/tc-18-2613-2024
- Glacier damage evolution over ice flow timescales M. Ranganathan et al. 10.5194/tc-19-1599-2025
- Topographic modulation of outlet glaciers in Greenland: a review G. Catania & D. Felikson 10.1017/aog.2023.55
- Predicting glacial lake outburst susceptibility on the southern Tibetan Plateau with historical events and machine learning methods H. Liu et al. 10.1007/s11069-025-07486-8
- Exploring potential glacial lakes using geo-spatial techniques in Eastern Hindu Kush Region, Pakistan M. Sarwar & S. Mahmood 10.1016/j.nhres.2023.07.003
- The Hunga Tonga–Hunga Haʻapai volcanic barometric pressure pulse and meteotsunami travel recorded in several Antarctic stations H. EVANGELISTA et al. 10.1590/0001-3765202420240556
Latest update: 23 Oct 2025
Co-editor-in-chief
This paper provides a complete and novel perspective on how to attribute changes in glaciers to anthropogenic warming. It is accessible, well written with clear figures, and will certainly be of interest to the wider community.
This paper provides a complete and novel perspective on how to attribute changes in glaciers to...
Short summary
Marine-terminating glaciers have recently retreated dramatically, but the role of anthropogenic forcing remains uncertain. We use idealized model simulations to develop a framework for assessing the probability of rapid retreat in the context of natural climate variability. Our analyses show that century-scale anthropogenic trends can substantially increase the probability of retreats. This provides a roadmap for future work to formally assess the role of human activity in recent glacier change.
Marine-terminating glaciers have recently retreated dramatically, but the role of anthropogenic...