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spelling ftinfoscience:oai:infoscience.epfl.ch:298312 2023-05-15T13:43:17+02:00 Eemian interglacial reconstructed from a Greenland folded ice core Dahl-Jensen, D. Albert, M. R. Aldahan, A. Azuma, N. Balslev-Clausen, D. Baumgartner, M. Berggren, A.-M. Bigler, M. Binder, T. Blunier, T. Bourgeois, J. C. Brook, E. J. Buchardt, S. L. Buizert, C. Capron, E. Chappellaz, J. Chung, J. Clausen, H. B. Cvijanovic, I. Davies, S. M. Ditlevsen, P. Eicher, O. Fischer, H. Fisher, D. A. Fleet, L. G. Gfeller, G. Gkinis, V. Gogineni, S. Goto-Azuma, K. Grinsted, A. Gudlaugsdottir, H. Guillevic, M. Hansen, S. B. Hansson, M. Hirabayashi, M. Hong, S. Hur, S. D. Huybrechts, P. Hvidberg, C. S. Iizuka, Y. Jenk, T. Johnsen, S. J. Jones, T. R. Jouzel, J. Karlsson, N. B. Kawamura, K. Keegan, K. Kettner, E. Kipfstuhl, S. Kjaer, H. A. 2022-11-23T16:11:19Z https://doi.org/10.1038/nature11789 http://infoscience.epfl.ch/record/298312 unknown London, Springer Science and Business Media LLC doi:10.1038/nature11789 isi:000313871400029 http://infoscience.epfl.ch/record/298312 http://infoscience.epfl.ch/record/298312 Text 2022 ftinfoscience https://doi.org/10.1038/nature11789 2023-02-13T23:12:29Z Efforts to extract a Greenland ice core with a complete record of the Eemian interglacial (130,000 to 115,000 years ago) have until now been unsuccessful. The response of the Greenland ice sheet to the warmer-than-present climate of the Eemian has thus remained unclear. Here we present the new North Greenland Eemian Ice Drilling ('NEEM') ice core and show only a modest ice-sheet response to the strong warming in the early Eemian. We reconstructed the Eemian record from folded ice using globally homogeneous parameters known from dated Greenland and Antarctic ice-core records. On the basis of water stable isotopes, NEEM surface temperatures after the onset of the Eemian (126,000 years ago) peaked at 8 ± 4 degrees Celsius above the mean of the past millennium, followed by a gradual cooling that was probably driven by the decreasing summer insolation. Between 128,000 and 122,000 years ago, the thickness of the northwest Greenland ice sheet decreased by 400 ± 250 metres, reaching surface elevations 122,000 years ago of 130 ± 300 metres lower than the present. Extensive surface melt occurred at the NEEM site during the Eemian, a phenomenon witnessed when melt layers formed again at NEEM during the exceptional heat of July 2012. With additional warming, surface melt might become more common in the future. © 2013 Macmillan Publishers Limited. All rights reserved. Text Antarc* Antarctic Greenland Greenland ice core ice core Ice Sheet North Greenland EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) Antarctic Greenland Nature 493 7433 489 494
institution Open Polar
collection EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne)
op_collection_id ftinfoscience
language unknown
description Efforts to extract a Greenland ice core with a complete record of the Eemian interglacial (130,000 to 115,000 years ago) have until now been unsuccessful. The response of the Greenland ice sheet to the warmer-than-present climate of the Eemian has thus remained unclear. Here we present the new North Greenland Eemian Ice Drilling ('NEEM') ice core and show only a modest ice-sheet response to the strong warming in the early Eemian. We reconstructed the Eemian record from folded ice using globally homogeneous parameters known from dated Greenland and Antarctic ice-core records. On the basis of water stable isotopes, NEEM surface temperatures after the onset of the Eemian (126,000 years ago) peaked at 8 ± 4 degrees Celsius above the mean of the past millennium, followed by a gradual cooling that was probably driven by the decreasing summer insolation. Between 128,000 and 122,000 years ago, the thickness of the northwest Greenland ice sheet decreased by 400 ± 250 metres, reaching surface elevations 122,000 years ago of 130 ± 300 metres lower than the present. Extensive surface melt occurred at the NEEM site during the Eemian, a phenomenon witnessed when melt layers formed again at NEEM during the exceptional heat of July 2012. With additional warming, surface melt might become more common in the future. © 2013 Macmillan Publishers Limited. All rights reserved.
format Text
author Dahl-Jensen, D.
Albert, M. R.
Aldahan, A.
Azuma, N.
Balslev-Clausen, D.
Baumgartner, M.
Berggren, A.-M.
Bigler, M.
Binder, T.
Blunier, T.
Bourgeois, J. C.
Brook, E. J.
Buchardt, S. L.
Buizert, C.
Capron, E.
Chappellaz, J.
Chung, J.
Clausen, H. B.
Cvijanovic, I.
Davies, S. M.
Ditlevsen, P.
Eicher, O.
Fischer, H.
Fisher, D. A.
Fleet, L. G.
Gfeller, G.
Gkinis, V.
Gogineni, S.
Goto-Azuma, K.
Grinsted, A.
Gudlaugsdottir, H.
Guillevic, M.
Hansen, S. B.
Hansson, M.
Hirabayashi, M.
Hong, S.
Hur, S. D.
Huybrechts, P.
Hvidberg, C. S.
Iizuka, Y.
Jenk, T.
Johnsen, S. J.
Jones, T. R.
Jouzel, J.
Karlsson, N. B.
Kawamura, K.
Keegan, K.
Kettner, E.
Kipfstuhl, S.
Kjaer, H. A.
spellingShingle Dahl-Jensen, D.
Albert, M. R.
Aldahan, A.
Azuma, N.
Balslev-Clausen, D.
Baumgartner, M.
Berggren, A.-M.
Bigler, M.
Binder, T.
Blunier, T.
Bourgeois, J. C.
Brook, E. J.
Buchardt, S. L.
Buizert, C.
Capron, E.
Chappellaz, J.
Chung, J.
Clausen, H. B.
Cvijanovic, I.
Davies, S. M.
Ditlevsen, P.
Eicher, O.
Fischer, H.
Fisher, D. A.
Fleet, L. G.
Gfeller, G.
Gkinis, V.
Gogineni, S.
Goto-Azuma, K.
Grinsted, A.
Gudlaugsdottir, H.
Guillevic, M.
Hansen, S. B.
Hansson, M.
Hirabayashi, M.
Hong, S.
Hur, S. D.
Huybrechts, P.
Hvidberg, C. S.
Iizuka, Y.
Jenk, T.
Johnsen, S. J.
Jones, T. R.
Jouzel, J.
Karlsson, N. B.
Kawamura, K.
Keegan, K.
Kettner, E.
Kipfstuhl, S.
Kjaer, H. A.
Eemian interglacial reconstructed from a Greenland folded ice core
author_facet Dahl-Jensen, D.
Albert, M. R.
Aldahan, A.
Azuma, N.
Balslev-Clausen, D.
Baumgartner, M.
Berggren, A.-M.
Bigler, M.
Binder, T.
Blunier, T.
Bourgeois, J. C.
Brook, E. J.
Buchardt, S. L.
Buizert, C.
Capron, E.
Chappellaz, J.
Chung, J.
Clausen, H. B.
Cvijanovic, I.
Davies, S. M.
Ditlevsen, P.
Eicher, O.
Fischer, H.
Fisher, D. A.
Fleet, L. G.
Gfeller, G.
Gkinis, V.
Gogineni, S.
Goto-Azuma, K.
Grinsted, A.
Gudlaugsdottir, H.
Guillevic, M.
Hansen, S. B.
Hansson, M.
Hirabayashi, M.
Hong, S.
Hur, S. D.
Huybrechts, P.
Hvidberg, C. S.
Iizuka, Y.
Jenk, T.
Johnsen, S. J.
Jones, T. R.
Jouzel, J.
Karlsson, N. B.
Kawamura, K.
Keegan, K.
Kettner, E.
Kipfstuhl, S.
Kjaer, H. A.
author_sort Dahl-Jensen, D.
title Eemian interglacial reconstructed from a Greenland folded ice core
title_short Eemian interglacial reconstructed from a Greenland folded ice core
title_full Eemian interglacial reconstructed from a Greenland folded ice core
title_fullStr Eemian interglacial reconstructed from a Greenland folded ice core
title_full_unstemmed Eemian interglacial reconstructed from a Greenland folded ice core
title_sort eemian interglacial reconstructed from a greenland folded ice core
publisher London, Springer Science and Business Media LLC
publishDate 2022
url https://doi.org/10.1038/nature11789
http://infoscience.epfl.ch/record/298312
geographic Antarctic
Greenland
geographic_facet Antarctic
Greenland
genre Antarc*
Antarctic
Greenland
Greenland ice core
ice core
Ice Sheet
North Greenland
genre_facet Antarc*
Antarctic
Greenland
Greenland ice core
ice core
Ice Sheet
North Greenland
op_source http://infoscience.epfl.ch/record/298312
op_relation doi:10.1038/nature11789
isi:000313871400029
http://infoscience.epfl.ch/record/298312
op_doi https://doi.org/10.1038/nature11789
container_title Nature
container_volume 493
container_issue 7433
container_start_page 489
op_container_end_page 494
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