Abstract
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.
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Acknowledgements
We thank the many persons involved in logistics, drill developments and drilling, and ice-core processing and analysis in the field and in our laboratories. NEEM is directed and organized by the Centre of Ice and Climate at the Niels Bohr Institute and US NSF, Office of Polar Programs. It is supported by funding agencies and institutions in Belgium (FNRS-CFB and FWO), Canada (NRCan/GSC), China (CAS), Denmark (FIST), France (IPEV, CNRS/INSU, CEA and ANR), Germany (AWI), Iceland (RannIs), Japan (NIPR), South Korea (KOPRI), The Netherlands (NWO/ALW), Sweden (VR), Switzerland (SNF), the United Kingdom (NERC) and the USA (US NSF, Office of Polar Programs) and the EU Seventh Framework programmes Past4Future and WaterundertheIce. NASA is acknowledged for the OIB 2011 programme.
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All authors contributed to the discussions that led to the results presented in the paper. M.R.A., A.-M.B., C.B., K. Keegan, P.M., S.B.S. and E.W. performed analysis and interpretation of the firn processes; A.A., D.B.-C., M. Baumgartner, M. Bigler, T. Blunier, E.J.B., E.C., J. Chappellaz, J. Chung, O.E., H.F., L.G.F., G.G., V.G., K.G.-A., M.H., Y.I., T.J., T.R.J., J.J., K. Kawamura, E.K., H.A.K., T.K., A.L., D.L., V.L., O.J.M., V.M.-D., J.R.M., O.M., R. Muscheler, J.-R.P., K.P., G.P., T.P., M.P., D.R., C.R., T.R., J.L.R., M.R., C.J.S., A.S., J.S., S. Schüpbach, J. P. Severinghaus, T.S., P.S., T.F.S., C.S., W.T.S., A.S.S., A. Sveinbjörnsdottir, A. Svensson, J.U., P.V., G.v.d.W., B.H.V., B.V., A.W. and F.W. were involved in the data measurements described in detail in Supplementary Information; N.A., T. Binder, S.K., A.M., M.M.-R., D.S., E.W. and I.W. contributed to the understanding of ice rheology; J.C.B. and A.M.Z.S. investigated the biology of the ice cores; S.L.B., P.H., M.K., F.P., A.Q., C.R., O.R., A.M.S. and R.S.W.v.d.W. produced ice-sheet models; H.B.C., S.M.D., D.A.F., A.G., H.G., M.G., S.J.J., P.K., A.L., T.L., M.L., S.O.R., I.S., J. P. Steffensen and M.W. participated in the dating of the NEEM ice core; I.C., P.D., P.L.L. and J.S. produced atmosphere models; D.D.-J. analysed the data; J.W.C.W. and E.W.W. put the discussion into the text; S.G., N.B.K., C.L., J.L., J.P., C. P. and D.S. participated in obtaining and interpreting the RES images; S.B.H. and S.S. were the chief mechanic and electronic engineer on the deep ice-core drill; M.G., S.H., S.D.H., H.M., R. Mulvaney, J.R. and C.X. participated in the planning of the NEEM project; L.B.L. and C.S.H. used a GPS net to determine the surface velocities; E.C., A.L., A.J.O., F.P., H.C.S.-L., K.S. and J.Z. participated in measuring temperatures and isotopes in the firn and air; J.-L.T. was involved in the interpretation of the basal ice.
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Supplementary Information
This file contains Supplementary Text and Data (see Content for details), Supplementary Figures 1-10, Supplementary Tables 1-2 and additional references. (PDF 1376 kb)
Supplementary Data
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NEEM community members. Eemian interglacial reconstructed from a Greenland folded ice core. Nature 493, 489–494 (2013). https://doi.org/10.1038/nature11789
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DOI: https://doi.org/10.1038/nature11789
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