Chinese Science Bulletin

, Volume 59, Issue 2, pp 201–211 | Cite as

Simulation of Greenland ice sheet during the mid-Pliocene warm period

Article Atmospheric Science

Abstract

One of the key uncertainties in future sea-level projections is attributed to the Greenland ice sheet (GrIS). Studying the response of the GrIS to climate changes during the past warm periods is helpful for understanding future changes in the GrIS. In this study, using three global climate models (Community Atmosphere Model version 3.1 and version 4.0 and Norwegian Earth System Model) and a three-dimensional ice sheet model, we investigate the climate and ice sheet changes over Greenland during the mid-Pliocene warm period (~3 Ma bp). The results show that the regionally averaged summer temperature over Greenland is 9.4–13.4 °C higher during the mid-Pliocene period than during the pre-industrial era and the annual mean precipitation is 65.2–108.3 mm a−1 greater. In response to this warm-wet climate, the GrIS shows a substantial decrease in size during the mid-Pliocene, with little ice existing along the eastern coast of Greenland. Compared to that simulated in the control run, the global sea level is approximately 7.8–8.1 m higher during the mid-Pliocene due to the decrease in the size of the GrIS. In addition, paleoclimate proxies also indicate that it is unlikely that a large-scale ice sheet exists over Greenland during the mid-Pliocene warm period.

Keywords

GrIS Mid-Pliocene Paleoclimate modeling Ice sheet modeling Paleoclimate proxies 

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Copyright information

© Science China Press and Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • Qing Yan
    • 1
    • 2
  • Zhongshi Zhang
    • 1
    • 3
  • Huijun Wang
    • 1
    • 4
  • Ran Zhang
    • 4
  1. 1.Nansen-Zhu International Research Centre, Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina
  2. 2.University of Chinese Academy of SciencesBeijingChina
  3. 3.Bjerknes Centre for Climate Research, UniResearchBergenNorway
  4. 4.Climate Change Research CenterChinese Academy of SciencesBeijingChina

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