Articles | Volume 12, issue 10
https://doi.org/10.5194/cp-12-2011-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-2011-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
28 Oct 2016
Research article |
| 28 Oct 2016
Warm Greenland during the last interglacial: the role of regional changes in sea ice cover
Niklaus Merz
CORRESPONDING AUTHOR
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Andreas Born
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Christoph C. Raible
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Thomas F. Stocker
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
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Cited
17 citations as recorded by crossref.
- On the causes of Arctic sea ice in the warm Early Pliocene C. Clotten et al. 10.1038/s41598-018-37047-y
- Sea ice feedbacks influence the isotopic signature of Greenland ice sheet elevation changes: last interglacial HadCM3 simulations I. Malmierca-Vallet et al. 10.5194/cp-16-2485-2020
- The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
- Simulating the Last Interglacial Greenland stable water isotope peak: The role of Arctic sea ice changes I. Malmierca-Vallet et al. 10.1016/j.quascirev.2018.07.027
- Dynamic boreal summer atmospheric circulation response as negative feedback to Greenland melt during the MIS-11 interglacial B. Crow et al. 10.5194/cp-18-775-2022
- Modeling the Greenland englacial stratigraphy A. Born & A. Robinson 10.5194/tc-15-4539-2021
- Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial R. Stein et al. 10.1038/s41467-017-00552-1
- Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model H. Goelzer et al. 10.5194/cp-12-2195-2016
- The role of land cover in the climate of glacial Europe P. Velasquez et al. 10.5194/cp-17-1161-2021
- Possible Role for Tectonics in the Evolving Stability of the Greenland Ice Sheet R. Alley et al. 10.1029/2018JF004714
- Attributing Greenland Warming Patterns to Regional Arctic Sea Ice Loss R. Pedersen & J. Christensen 10.1029/2019GL083828
- Eemian Greenland SMB strongly sensitive to model choice A. Plach et al. 10.5194/cp-14-1463-2018
- Tracer transport in an isochronal ice-sheet model A. BORN 10.1017/jog.2016.111
- A seasonally ice-free Arctic Ocean during the Last Interglacial F. Vermassen et al. 10.1038/s41561-023-01227-x
- How warm was Greenland during the last interglacial period? A. Landais et al. 10.5194/cp-12-1933-2016
- Perspective of Isotope Hydrometeorology K. YOSHIMURA 10.3178/jjshwr.31.554
- Greenland during the last interglacial: the relative importance of insolation and oceanic changes R. Pedersen et al. 10.5194/cp-12-1907-2016
14 citations as recorded by crossref.
- On the causes of Arctic sea ice in the warm Early Pliocene C. Clotten et al. 10.1038/s41598-018-37047-y
- Sea ice feedbacks influence the isotopic signature of Greenland ice sheet elevation changes: last interglacial HadCM3 simulations I. Malmierca-Vallet et al. 10.5194/cp-16-2485-2020
- The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
- Simulating the Last Interglacial Greenland stable water isotope peak: The role of Arctic sea ice changes I. Malmierca-Vallet et al. 10.1016/j.quascirev.2018.07.027
- Dynamic boreal summer atmospheric circulation response as negative feedback to Greenland melt during the MIS-11 interglacial B. Crow et al. 10.5194/cp-18-775-2022
- Modeling the Greenland englacial stratigraphy A. Born & A. Robinson 10.5194/tc-15-4539-2021
- Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial R. Stein et al. 10.1038/s41467-017-00552-1
- Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model H. Goelzer et al. 10.5194/cp-12-2195-2016
- The role of land cover in the climate of glacial Europe P. Velasquez et al. 10.5194/cp-17-1161-2021
- Possible Role for Tectonics in the Evolving Stability of the Greenland Ice Sheet R. Alley et al. 10.1029/2018JF004714
- Attributing Greenland Warming Patterns to Regional Arctic Sea Ice Loss R. Pedersen & J. Christensen 10.1029/2019GL083828
- Eemian Greenland SMB strongly sensitive to model choice A. Plach et al. 10.5194/cp-14-1463-2018
- Tracer transport in an isochronal ice-sheet model A. BORN 10.1017/jog.2016.111
- A seasonally ice-free Arctic Ocean during the Last Interglacial F. Vermassen et al. 10.1038/s41561-023-01227-x
3 citations as recorded by crossref.
- How warm was Greenland during the last interglacial period? A. Landais et al. 10.5194/cp-12-1933-2016
- Perspective of Isotope Hydrometeorology K. YOSHIMURA 10.3178/jjshwr.31.554
- Greenland during the last interglacial: the relative importance of insolation and oceanic changes R. Pedersen et al. 10.5194/cp-12-1907-2016
Saved (preprint)
Latest update: 14 Dec 2024
Short summary
The last (Eemian) interglacial is studied with a global climate model focusing on Greenland and the adjacent high latitudes. A set of model experiments demonstrates the crucial role of changes in sea ice and sea surface temperatures for the magnitude of Eemian atmospheric warming. Greenland temperatures are found highly sensitive to sea ice changes in the Nordic Seas but rather insensitive to changes in the Labrador Sea. This behavior has important implications for Greenland ice core signals.
The last (Eemian) interglacial is studied with a global climate model focusing on Greenland and...
