Articles | Volume 15, issue 12
https://doi.org/10.5194/tc-15-5739-2021
© Author(s) 2021. 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-15-5739-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
20 Dec 2021
Research article | Highlight paper |
| 20 Dec 2021
| 20 Dec 2021
Impact of the melt–albedo feedback on the future evolution of the Greenland Ice Sheet with PISM-dEBM-simple
Maria Zeitz
CORRESPONDING AUTHOR
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
Institute of Physics and Astronomy, University of Potsdam, Karl-Liebknecht-Str. 24–25, 14476 Potsdam, Germany
Ronja Reese
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
Johanna Beckmann
Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, P.O. Box 60 12 03, 14412 Potsdam, Germany
Uta Krebs-Kanzow
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
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
Institute of Physics and Astronomy, University of Potsdam, Karl-Liebknecht-Str. 24–25, 14476 Potsdam, Germany
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Cited
16 citations as recorded by crossref.
- Effects of increasing soil moisture on Antarctic desert microbial ecosystems E. Zhang et al. 10.1111/cobi.14268
- 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
- Improving modelled albedo over the Greenland ice sheet through parameter optimisation and MODIS snow albedo retrievals N. Raoult et al. 10.5194/tc-17-2705-2023
- A topographically controlled tipping point for complete Greenland ice sheet melt M. Petrini et al. 10.5194/tc-19-63-2025
- Review of Land Surface Albedo: Variance Characteristics, Climate Effect and Management Strategy X. Zhang et al. 10.3390/rs14061382
- The long-term sea-level commitment from Antarctica A. Klose et al. 10.5194/tc-18-4463-2024
- Overshooting the critical threshold for the Greenland ice sheet N. Bochow et al. 10.1038/s41586-023-06503-9
- The evolution of future Antarctic surface melt using PISM-dEBM-simple J. Garbe et al. 10.5194/tc-17-4571-2023
- Smartphone-based measurements of the optical properties of snow M. Allgaier & B. Smith 10.1364/AO.457976
- Author Correction: Overshooting the critical threshold for the Greenland ice sheet N. Bochow et al. 10.1038/s41586-023-06852-5
- Disentangling the drivers of future Antarctic ice loss with a historically calibrated ice-sheet model V. Coulon et al. 10.5194/tc-18-653-2024
- Contribution of surface and cloud radiative feedbacks to Greenland Ice Sheet meltwater production during 2002–2023 J. Ryan 10.1038/s43247-024-01714-y
- Projections of precipitation and temperatures in Greenland and the impact of spatially uniform anomalies on the evolution of the ice sheet N. Bochow et al. 10.5194/tc-18-5825-2024
- Deglaciation of northwestern Greenland during Marine Isotope Stage 11 A. Christ et al. 10.1126/science.ade4248
- Temporal variability in air temperature lapse rates across the glacierised terrain of the Chandra basin, western Himalaya S. Oulkar et al. 10.1007/s00704-024-05003-8
- Role of Snowfall Versus Air Temperatures for Greenland Ice Sheet Melt‐Albedo Feedbacks J. Ryan et al. 10.1029/2023EA003158
16 citations as recorded by crossref.
- Effects of increasing soil moisture on Antarctic desert microbial ecosystems E. Zhang et al. 10.1111/cobi.14268
- 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
- Improving modelled albedo over the Greenland ice sheet through parameter optimisation and MODIS snow albedo retrievals N. Raoult et al. 10.5194/tc-17-2705-2023
- A topographically controlled tipping point for complete Greenland ice sheet melt M. Petrini et al. 10.5194/tc-19-63-2025
- Review of Land Surface Albedo: Variance Characteristics, Climate Effect and Management Strategy X. Zhang et al. 10.3390/rs14061382
- The long-term sea-level commitment from Antarctica A. Klose et al. 10.5194/tc-18-4463-2024
- Overshooting the critical threshold for the Greenland ice sheet N. Bochow et al. 10.1038/s41586-023-06503-9
- The evolution of future Antarctic surface melt using PISM-dEBM-simple J. Garbe et al. 10.5194/tc-17-4571-2023
- Smartphone-based measurements of the optical properties of snow M. Allgaier & B. Smith 10.1364/AO.457976
- Author Correction: Overshooting the critical threshold for the Greenland ice sheet N. Bochow et al. 10.1038/s41586-023-06852-5
- Disentangling the drivers of future Antarctic ice loss with a historically calibrated ice-sheet model V. Coulon et al. 10.5194/tc-18-653-2024
- Contribution of surface and cloud radiative feedbacks to Greenland Ice Sheet meltwater production during 2002–2023 J. Ryan 10.1038/s43247-024-01714-y
- Projections of precipitation and temperatures in Greenland and the impact of spatially uniform anomalies on the evolution of the ice sheet N. Bochow et al. 10.5194/tc-18-5825-2024
- Deglaciation of northwestern Greenland during Marine Isotope Stage 11 A. Christ et al. 10.1126/science.ade4248
- Temporal variability in air temperature lapse rates across the glacierised terrain of the Chandra basin, western Himalaya S. Oulkar et al. 10.1007/s00704-024-05003-8
- Role of Snowfall Versus Air Temperatures for Greenland Ice Sheet Melt‐Albedo Feedbacks J. Ryan et al. 10.1029/2023EA003158
Latest update: 20 Jan 2025
Short summary
With the increasing melt of the Greenland Ice Sheet, which contributes to sea level rise, the surface of the ice darkens. The dark surfaces absorb more radiation and thus experience increased melt, resulting in the melt–albedo feedback. Using a simple surface melt model, we estimate that this positive feedback contributes to an additional 60 % ice loss in a high-warming scenario and additional 90 % ice loss for moderate warming. Albedo changes are important for Greenland’s future ice loss.
With the increasing melt of the Greenland Ice Sheet, which contributes to sea level rise, the...
