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The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr

  • LISBETH T. NIELSEN (a1), GUðFINNA AÐALGEIRSDÓTTIR (a2), VASILEIOS GKINIS (a1), ROMAN NUTERMAN (a3) and CHRISTINE S. HVIDBERG (a1)...
Abstract

The Holocene climatic optimum was a period 8–5 kyr ago when annual mean surface temperatures in Greenland were 2–3°C warmer than present-day values. However, this warming left little imprint on commonly used temperature proxies often used to derive the climate forcing for simulations of the past evolution of the Greenland ice sheet. In this study, we investigate the evolution of the Greenland ice sheet through the Holocene when forced by different proxy-derived temperature histories from ice core records, focusing on the effect of sustained higher surface temperatures during the early Holocene. We find that the ice sheet retreats to a minimum volume of ~0.15–1.2 m sea-level equivalent smaller than present in the early or mid-Holocene when forcing an ice-sheet model with temperature reconstructions that contain a climatic optimum, and that the ice sheet has continued to recover from this minimum up to present day. Reconstructions without a warm climatic optimum in the early Holocene result in smaller ice losses continuing throughout the last 10 kyr. For all the simulated ice-sheet histories, the ice sheet is approaching a steady state at the end of the 20th century.

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Copyright
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Corresponding author
Correspondence: Christine S. Hvidberg <ch@nbi.ku.dk>
References
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Abe-Ouchi, A, Segawa, T and Saito, F (2007) Climatic conditions for modelling the Northern Hemisphere ice sheets throughout the ice age cycle. Clim. Past, 3(1), 301336 (doi: 10.5194/cpd-3-301-2007)
Aðalgeirsdóttir, G and 6 others (2014) Role of model initialization for projections of 21st-century Greenland ice sheet mass loss. J. Glaciol., 60(222), 782794 (doi: 10.3189/2014JoG13J202)
Arthern, R and Gudmundsson, G (2010) Initialization of ice-sheet forecasts viewed as an inverse Robin problem. J. Glaciol., 56, 527533 (doi: 10.3189/002214310792447699)
Aschwanden, A, Fahnestock, M and Truffer, M (2016) Complex Greenland outlet glacier flow captured. Nat. Commun., 7 (doi: 10.1038/ncomms10524)
Bamber, J and 5 others (2013) A new bed elevation dataset for Greenland. Cryosphere, 7(2), 499510 (doi: 10.5194/tc-7-499-2013)
Bindschadler, R and 27 others (2013) Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project). J. Glaciol., 59(214), 195224 (doi: 10.3189/2013JoG12J125)
Bueler, E and Brown, J (2009) Shallow shelf approximation as a “sliding law” in a thermomechanically coupled ice sheet model. J. Geophys. Res., 114 (doi: 10.1029/2008JF001179)
Calov, R and Greve, R (2005) A semi-analytical solution for the positive degree-day model with stochastic temperature variations. J. Glaciol., 51(172), 173175 (doi: 10.3189/172756505781829601)
Clarke, G, Lhomme, N and Marshall, S (2005) Tracer transport in the Greenland ice sheet: three-dimensional isotopic stratigraphy. Quat. Sci. Rev., 24, 155171 (doi: 10.1016/j.quascirev.2004.08.021)
Cuffey, K and Clow, G (1997) Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition. J. Geophys. Res., 102, 383396
Cuffey, K and Marshall, S (2000) Substantial contribution to sea-level rise during the last interglacial from the Greenland ice sheet. Nature, 404, 591594
Dahl-Jensen, D (1985) Determination of the flow properties at Dye 3, south Greenland, by bore-hole-tilting measurements and perturbation modelling. J. Glaciol., 31(108), 9298
Dahl-Jensen, D and 6 others (1998) Past temperatures Directly from the Greenland ice sheet. Science, 282(5387), 268271 (doi: 10.1126/science.282.5387.268)
Dansgaard, W (1964) Stable isotopes on precipitation. Tellus, 16
Dansgaard, W and 10 others (1993) Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 364, 218220
Funder, S, Kjeldsen, K, Kjær, K and Cofaigh, C (2011) The Greenland ice sheet during the past 300,000 years: a review. In Ehlers, J, Gibbard, P and Hughes, PD Eds, Quaternary glaciations – extent and chronology - a closer look, Developments in Quaternary Science 15. Elsevier, 699713 (doi: 10.1016/B978-0-444-53447-7.00050-7)
Gkinis, V, Simonsen, S, Buchardt, S, White, J and Vinther, B (2014) Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years- Glaciological and paleoclimatic implications. Earth. Planet. Sci. Lett., 405, 132141 (doi: 10.1016/j.epsl.2014.08.022)
Goelzer, H and 8 others (2013) Sensitivity of Greenland ice sheet projections to model formulations. J. Glaciol., 59(216), 733749 (doi: 10.3189/2013JoG12J182)
Greve, R, Saito, F and Abe-Ouchi, A (2011) Initial results of the SeaRISE numerical experiments with the models SICOPOLIC and IcIES for the Greenland ice sheet. Ann. Glaciol., 52(58), 2330 (doi: 10.3189/172756411797252068)
Gundestrup, N, Dahl-Jsense, D, Hansen, B and Kelty, J (1993) Bore-hole survey at Camp Century, 1989. Cold. Reg. Sci. Technol., 21, 187193
Hutter, K (1983) Theoritical glaciology: material science of ice and the mechanics of glaciers and ice sheets. D. Reidel, Dordrecht/Terra Scientific, Tokyo. (doi: 10.1007/978-94-015-1167-4)
Huybrechts, P (1998) Report of the Third EISMINT Workshop on Model Intercomparison. Tech. rep., Grindelwald, Switzerland.
Huybrechts, P (2002) Sea-level changes at the LGM from ice-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles. Quat. Sci. Rev., 21, 203231
Imbrie, J and 8 others (1984) The Orbital Theory of Pleistocene Climate: Support from a Revised Chronology of the Marine δ 18O Record
Johnsen, S and Vinther, B (2007) Greenland stable isotopes. In Elias, Scott A, ed., Enclyclopedia of quaternary science, 12501258, Elsevier
Johnsen, S, Dahl-Jensen, D, Dansgaard, W and Gundestrup, N (1995) Greenland palaeotemperatures derived from GRIP bore hole temperature and ice core isotope profiles. Tellus, 47B, 624629
Johnsen, S and 14 others (1997) The δ 18o record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability. J. Geophys. Res., 102(C12), 2639726410
Jouzel, J and 12 others (1997) Validity of the temperature reconstruction from ice cores. J. Geophys. Res., 102(C12), 2647126487
Kaufman, D and 29 others (2004) Holocene thermal maximum in the western Arctic (0-180°W). Quat. Sci. Rev., 23(5–6), 529560 (doi: 10.1016/j.quascirev.2003.09.007)
Khan, S and 5 others (2008) Geodetic measurements of postglacial adjustments in Greenland. J. Geophys. Res., 113, B02402 (doi: 10.1029/2007JB004956)
Lecavalier, B and 11 others (2014) A model of Greenland ice sheet deglaciation constrained by observations of relative sea level and ice extent. Quat. Sci. Rev., 102, 5484 (doi: 10.1016/j.quascirev.2014.07.018)
MacGregor, JA and 6 others (2016) Holocene deceleration of the Greenland Ice Sheet. Science, 351(6273), 590593 (doi: 10.1126/science.aab1702)
Moon, T, Joughin, I, Smith, B and Howat, I (2012) 21st-Century Evolution of Greenland Outlet Glacier Velocities. Science, 336, 576578 (doi: 10.1126/science.1219985)
Morland, LW (1987) Unconfined ice-shelf flow. In van der Veen, C and Oerlemans, J, eds. Dynamics of the West Antarctic Ice Sheet. Glaciology and Quaternary Geology, vol. 4. Springer, Dordrecht (doi: https://doi.org/10.1007/978-94-009-3745-1_6)
Morlighem, M, Rignot, E, Mouginot, J, Seroussi, H and Larour, E (2014) Deeply incised submarine glacial valleys beneath the Greenland ice sheet. Nat. Geosci., 7, 1822 (doi: 10.1038/NGEO2167)
NGRIP Members (2004) High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature, 431, 147151 (doi: 10.1038/nature02805)
Noël, B and 5 others (2015) Evaluation of the updated regional climate model RACMO2.3: Summer snowfall impact on the Greenland Ice Sheet. The Cryosphere, 9(5), 18311844 (doi: 10.5194/tc-9-1831-2015)
Nowicki, S and 30 others (2013) Insights into spatial sensitivities of ice mass response to environmental change from the SeaRISE ice sheet modeling project II: Greenland. J. Geophys. Res., 118(2), 10251044 (doi: 10.1002/jgrf.20076)
Nowicki, S and 8 others (2016) Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6. Geoscientific Model Development Discussions, 142 (doi: 10.5194/gmd-2016-105)
Peano, D, Colleoni, F, Quiquet, A and Masina, S (2017) Ice flux evolution in fast flowing areas of the Greenland ice sheet over the 20th and 21st centuries. J. Glaciol., 63(239), 499513 (doi: 10.1017/jog.2017.12)
Reeh, N (1991) Parameterization of melt rate and surface temperature on the Greenland ice sheet. Polarforschung, 59(3), 113128
Ridley, J, Huybrechts, P, Gregory, J and Lowe, J (2005) Elimination of the Greenland Ice Sheet in a High CO2 Climate. J. Clim., 18(17), 34093427 (doi: 10.1175/JCLI3482.1)
Ridley, J, Gregory, J, Huybrechts, P and Lowe, J (2009) Thresholds for irreversible decline of the greenland ice sheet. Clim. Dyn., 35(6), 10491057 (doi: 10.1007/s00382-009-0646-0)
Rignot, E, Velicogna, I, van den, Broeke M, Monaghan, A and Lenaerts, J (2011) Acceleration of the contribution of the Greenland and Antarctic ice sheets to sea level rise. Geophys. Res. Lett., 38 (doi: 10.1029/2011GL046583)
Rogozhina, I, Martinec, Z, Hagedoorn, J, Thomas, M and Fleming, K (2011) On the long-term memory of the Greenland Ice Sheet. J. Geophys. Res., 116(F1) (doi: 10.1029/2010JF001787)
Seierstad, I and 19 others (2014) Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ 18O gradients with possible Heinrich event imprint. Quat. Sci. Rev., 106, 2946 (doi: 10.1016/j.quascirev.2014.10.032)
Shepherd, A and 46 others (2012) A Reconciled Estimate of Ice-Sheet Mass Balance. Science, 338, 11831189 (doi: 10.1126/science.1228102)
Tarasov, L and Peltier, W (2002) Greenland glacial history and local geodynamic consequences. Geophys. J. Int., 150, 198229
Tarasov, L and Peltier, W (2003) Greenland glacial history, borehole constraints, and Eemian extent. J. Geophys. Res., 108(B3) (doi: 10.1029/2001JB001731)
The PISM authors (2016) PISM, a Parallel Ice Sheet Mode. http://www.pism-docs.org
Thorsteinsson, T, Waddington, E, Taylor, K, Alley, R and Blankenship, D (1999) Strain-rate enhancement at Dye 3, Greenland. J. Glaciol., 45(150), 338345
Vinther, B and 13 others (2009) Holocene thinning of the Greenland ice sheet. Nature, 461(7262), 385388 (doi: 10.1038/nature08355)
Vizcaino, M and 5 others (2015) Coupled simulations of Greenland Ice Sheet and climate change up to A.D. 2300. Geophys. Res. Lett., 42, 39273935 (doi: 10.1002/2014GL061142)
White, J and 8 others (2010) Past rates of climate change in the Arctic. Quat. Sci. Rev., 29(15–16), 17161727 (doi: 10.1016/j.quascirev.2010.04.025)
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