globalchange  > 气候变化与战略
DOI: 10.1073/pnas.1524766113
论文题名:
Reconstructing the last interglacial at Summit; Greenland: Insights from GISP2
作者: Yau A.M.; Bender M.L.; Robinson A.; Brook E.J.
刊名: Proceedings of the National Academy of Sciences of the United States of America
ISSN: 0027-8424
出版年: 2016
卷: 113, 期:35
起始页码: 9710
结束页码: 9715
语种: 英语
英文关键词: Greenland ice sheet ; Ice cores ; Last interglacial ; Sea level rise
Scopus关键词: ice ; nitrogen 15 ; oxygen ; oxygen 18 ; air ; Article ; climate ; climate change ; environmental temperature ; greenhouse effect ; Greenland ; interglacial ; priority journal ; sea level ; simulation ; warming
英文摘要: The Eemian (last interglacial, 130-115 ka) was likely the warmest of all interglacials of the last 800 ka, with summer Arctic temperatures 3-5 °C above present. Here, we present improved Eemian climate records from central Greenland, reconstructed from the base of the Greenland Ice Sheet Project 2 (GISP2) ice core. Our record comes from clean, stratigraphically disturbed, and isotopi-cally warm ice from 2, 750 to 3, 040 m depth. The age of this ice is constrained by measuring CH4 and δ18O of O2, and comparing with the historical record of these properties from the North Greenland Ice Core Project (NGRIP) and North Greenland Eemian Ice Drilling (NEEM) ice cores. The δ18Oice, δ15N of N2, and total air content for samples dating discontinuously from 128 to 115 ka indicate a warming of ∼6 °C between 127-121 ka, and a similar elevation history between GISP2 and NEEM. The reconstructed climate and elevation histories are compared with an ensemble of coupled climate-ice-sheet model simulations of the Greenland ice sheet. Those most consistent with the reconstructed temperatures indicate that the Greenland ice sheet contributed 5.1 m (4.1-6.2 m, 95% credible interval) to global eustatic sea level toward the end of the Eemian. Greenland likely did not contribute to anomalously high sea levels at ∼127 ka, or to a rapid jump in sea level at ∼120 ka. However, several unexplained discrepancies remain between the inferred and simulated histories of temperature and accumulation rate at GISP2 and NEEM, as well as between the climatic reconstructions themselves.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/162119
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作者单位: Yau, A.M., Department of Geosciences, Princeton University, Princeton, NJ 08540, United States; Bender, M.L., Department of Geosciences, Princeton University, Princeton, NJ 08540, United States, Institute of Oceanology, Shanghai Jiao Tong University, Minhang District, Shanghai, 200240, China; Robinson, A., Universidad Complutense de Madrid, Madrid, 28040, Spain, Instituto de Geociencias, Universidad Complutense de Madrid, Consejo Superior de Investigaciones Científicas, Madrid, 28040, Spain, Potsdam Institute for Climate Impact Research, Potsdam, 14473, Germany; Brook, E.J., College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States

Recommended Citation:
Yau A.M.,Bender M.L.,Robinson A.,et al. Reconstructing the last interglacial at Summit; Greenland: Insights from GISP2[J]. Proceedings of the National Academy of Sciences of the United States of America,2016-01-01,113(35)
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