Articles | Volume 14, issue 10
https://doi.org/10.5194/cp-14-1463-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-1463-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
19 Oct 2018
Research article |
| 19 Oct 2018
| 19 Oct 2018
Eemian Greenland SMB strongly sensitive to model choice
Department of Earth Science, University of Bergen and Bjerknes Centre for Climate Research, Bergen,
Norway
Kerim H. Nisancioglu
Department of Earth Science, University of Bergen and Bjerknes Centre for Climate Research, Bergen,
Norway
Centre for Earth Evolution and Dynamics, University of Oslo,
Oslo, Norway
Sébastien Le clec'h
Laboratoire des Sciences du Climat et de l'Environnement,
LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 91191
Gif-sur-Yvette, France
Earth System Science and Department Geografie, Vrije Universiteit Brussel, Brussels, Belgium
Andreas Born
Department of Earth Science, University of Bergen and Bjerknes Centre for Climate Research, Bergen,
Norway
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Petra M. Langebroek
Uni Research Climate and Bjerknes Centre for Climate Research, Bergen, Norway
Chuncheng Guo
Uni Research Climate and Bjerknes Centre for Climate Research, Bergen, Norway
Michael Imhof
Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zürich, Switzerland
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Thomas F. Stocker
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
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Cited
14 citations as recorded by crossref.
- Present day Jakobshavn Isbræ (West Greenland) close to the Holocene minimum extent K. Kajanto et al. 10.1016/j.quascirev.2020.106492
- An efficient surface energy–mass balance model for snow and ice A. Born et al. 10.5194/tc-13-1529-2019
- Brief communication: An ice surface melt scheme including the diurnal cycle of solar radiation U. Krebs-Kanzow et al. 10.5194/tc-12-3923-2018
- Eemian Greenland ice sheet simulated with a higher-order model shows strong sensitivity to surface mass balance forcing A. Plach et al. 10.5194/tc-13-2133-2019
- A low climate threshold for south Greenland Ice Sheet demise during the Late Pleistocene N. Irvalı et al. 10.1073/pnas.1911902116
- Oceanic forcing of penultimate deglacial and last interglacial sea-level rise P. Clark et al. 10.1038/s41586-020-1931-7
- Modeling the Greenland englacial stratigraphy A. Born & A. Robinson 10.5194/tc-15-4539-2021
- Subglacial valleys preserved in the highlands of south and east Greenland record restricted ice extent during past warmer climates G. Paxman et al. 10.5194/tc-18-1467-2024
- The diurnal Energy Balance Model (dEBM): a convenient surface mass balance solution for ice sheets in Earth system modeling U. Krebs-Kanzow et al. 10.5194/tc-15-2295-2021
- Rapid Laurentide Ice Sheet growth preceding the Last Glacial Maximum due to summer snowfall L. Niu et al. 10.1038/s41561-024-01419-z
- Greenland Ice Sheet Surface Runoff Projections to 2200 Using Degree-Day Methods C. Yue et al. 10.3390/atmos12121569
- Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
- Drill-site selection for cosmogenic-nuclide exposure dating of the bed of the Greenland Ice Sheet J. Briner et al. 10.5194/tc-16-3933-2022
- Greenland climate simulations show high Eemian surface melt which could explain reduced total air content in ice cores A. Plach et al. 10.5194/cp-17-317-2021
14 citations as recorded by crossref.
- Present day Jakobshavn Isbræ (West Greenland) close to the Holocene minimum extent K. Kajanto et al. 10.1016/j.quascirev.2020.106492
- An efficient surface energy–mass balance model for snow and ice A. Born et al. 10.5194/tc-13-1529-2019
- Brief communication: An ice surface melt scheme including the diurnal cycle of solar radiation U. Krebs-Kanzow et al. 10.5194/tc-12-3923-2018
- Eemian Greenland ice sheet simulated with a higher-order model shows strong sensitivity to surface mass balance forcing A. Plach et al. 10.5194/tc-13-2133-2019
- A low climate threshold for south Greenland Ice Sheet demise during the Late Pleistocene N. Irvalı et al. 10.1073/pnas.1911902116
- Oceanic forcing of penultimate deglacial and last interglacial sea-level rise P. Clark et al. 10.1038/s41586-020-1931-7
- Modeling the Greenland englacial stratigraphy A. Born & A. Robinson 10.5194/tc-15-4539-2021
- Subglacial valleys preserved in the highlands of south and east Greenland record restricted ice extent during past warmer climates G. Paxman et al. 10.5194/tc-18-1467-2024
- The diurnal Energy Balance Model (dEBM): a convenient surface mass balance solution for ice sheets in Earth system modeling U. Krebs-Kanzow et al. 10.5194/tc-15-2295-2021
- Rapid Laurentide Ice Sheet growth preceding the Last Glacial Maximum due to summer snowfall L. Niu et al. 10.1038/s41561-024-01419-z
- Greenland Ice Sheet Surface Runoff Projections to 2200 Using Degree-Day Methods C. Yue et al. 10.3390/atmos12121569
- Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
- Drill-site selection for cosmogenic-nuclide exposure dating of the bed of the Greenland Ice Sheet J. Briner et al. 10.5194/tc-16-3933-2022
- Greenland climate simulations show high Eemian surface melt which could explain reduced total air content in ice cores A. Plach et al. 10.5194/cp-17-317-2021
Latest update: 23 Apr 2024
Short summary
The Greenland ice sheet is a huge frozen water reservoir which is crucial for predictions of sea level in a warming future climate. Therefore, computer models are needed to reliably simulate the melt of ice sheets. In this study, we use climate model simulations of the last period where it was warmer than today in Greenland. We test different melt models under these climatic conditions and show that the melt models show very different results under these warmer conditions.
The Greenland ice sheet is a huge frozen water reservoir which is crucial for predictions of sea...
