Sensitivity of the North Atlantic climate to Greenland Ice Sheet melting during the Last Interglacial
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Sensitivity of the North Atlantic climate to Greenland Ice Sheet melting during the Last Interglacial ; volume:8 ; number:3 ; year:2012 ; pages:995-1009
Climate of the past ; 8, Heft 3 (2012), 995-1009
- Creator
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Bakker, P.
Van Meerbeeck, C. J.
Renssen, H.
- DOI
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10.5194/cp-8-995-2012
- URN
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urn:nbn:de:101:1-201710277206
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:29 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Bakker, P.
- Van Meerbeeck, C. J.
- Renssen, H.
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Dissolved organic nutrients dominate melting surface ice of the Dark Zone (Greenland Ice Sheet)
How warm was Greenland during the last interglacial period?
Sea-ice feedbacks influence the isotopic signature of Greenland Ice Sheet elevation changes: Last Interglacial HadCM3 simulations
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Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model
Moderate Greenland ice sheet melt during the last interglacial constrained by present-day observations and paleo ice core reconstructions
Unprecedented atmospheric conditions (1948–2019) drive the 2019 exceptional melting season over the Greenland ice sheet
Atlantic deep water circulation during the last interglacial
Greenland ice sheet model parameters constrained using simulations of the Eemian Interglacial
The sensitivity of the Greenland ice sheet to glacial-interglacial oceanic forcing
Quantification of the Greenland ice sheet contribution to Last Interglacial sea level rise
Persistent influence of ice sheet melting on high northern latitude climate during the early Last Interglacial
Dissolved organic nutrients dominate melting surface ice of the Dark Zone (Greenland Ice Sheet)
How warm was Greenland during the last interglacial period?
Sea-ice feedbacks influence the isotopic signature of Greenland Ice Sheet elevation changes: Last Interglacial HadCM3 simulations
Sea ice feedbacks influence the isotopic signature of Greenland ice sheet elevation changes: last interglacial HadCM3 simulations
Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model
Moderate Greenland ice sheet melt during the last interglacial constrained by present-day observations and paleo ice core reconstructions
Unprecedented atmospheric conditions (1948–2019) drive the 2019 exceptional melting season over the Greenland ice sheet
Atlantic deep water circulation during the last interglacial
Greenland ice sheet model parameters constrained using simulations of the Eemian Interglacial
The sensitivity of the Greenland ice sheet to glacial-interglacial oceanic forcing
Quantification of the Greenland ice sheet contribution to Last Interglacial sea level rise
Persistent influence of ice sheet melting on high northern latitude climate during the early Last Interglacial
Dissolved organic nutrients dominate melting surface ice of the Dark Zone (Greenland Ice Sheet)
How warm was Greenland during the last interglacial period?
Sea-ice feedbacks influence the isotopic signature of Greenland Ice Sheet elevation changes: Last Interglacial HadCM3 simulations
Sea ice feedbacks influence the isotopic signature of Greenland ice sheet elevation changes: last interglacial HadCM3 simulations
Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model
Moderate Greenland ice sheet melt during the last interglacial constrained by present-day observations and paleo ice core reconstructions
Unprecedented atmospheric conditions (1948–2019) drive the 2019 exceptional melting season over the Greenland ice sheet