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DOI | 10.1073/pnas.1807261116 |
Impact of abrupt sea ice loss on Greenland water isotopes during the last glacial period | |
Sime L.C.; Hopcroft P.O.; Rhodes R.H. | |
发表日期 | 2019 |
ISSN | 0027-8424 |
起始页码 | 4099 |
结束页码 | 4104 |
卷号 | 116期号:10 |
英文摘要 | Greenland ice cores provide excellent evidence of past abrupt climate changes. However, there is no universally accepted theory of how and why these Dansgaard–Oeschger (DO) events occur. Several mechanisms have been proposed to explain DO events, including sea ice, ice shelf buildup, ice sheets, atmospheric circulation, and meltwater changes. DO event temperature reconstructions depend on the stable water isotope (δ 18 O) and nitrogen isotope measurements from Greenland ice cores: interpretation of these measurements holds the key to understanding the nature of DO events. Here, we demonstrate the primary importance of sea ice as a control on Greenland ice core δ 18 O: 95% of the variability in δ 18 O in southern Greenland is explained by DO event sea ice changes. Our suite of DO events, simulated using a general circulation model, accurately captures the amplitude of δ 18 O enrichment during the abrupt DO event onsets. Simulated geographical variability is broadly consistent with available ice core evidence. We find an hitherto unknown sensitivity of the δ 18 O paleothermometer to the magnitude of DO event temperature increase: the change in δ 18 O per Kelvin temperature increase reduces with DO event amplitude. We show that this effect is controlled by precipitation seasonality. © 2019 National Academy of Sciences. All Rights Reserved. |
英文关键词 | Abrupt warmings; Arctic; climate change; paleoclimate; sea ice |
语种 | 英语 |
scopus关键词 | oxygen 18; Article; controlled study; glacial period; Greenland; mathematical model; measurement accuracy; precipitation; priority journal; sea ice; seasonal variation; temperature |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/160425 |
作者单位 | Sime, L.C., Ice Dynamics and Palaeoclimate, British Antarctic Survey, Cambridge, CB3 0ET, United Kingdom; Hopcroft, P.O., School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, B15 2TT, United Kingdom; Rhodes, R.H., Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, United Kingdom, Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne, NE1 8ST, United Kingdom |
推荐引用方式 GB/T 7714 | Sime L.C.,Hopcroft P.O.,Rhodes R.H.. Impact of abrupt sea ice loss on Greenland water isotopes during the last glacial period[J],2019,116(10). |
APA | Sime L.C.,Hopcroft P.O.,&Rhodes R.H..(2019).Impact of abrupt sea ice loss on Greenland water isotopes during the last glacial period.Proceedings of the National Academy of Sciences of the United States of America,116(10). |
MLA | Sime L.C.,et al."Impact of abrupt sea ice loss on Greenland water isotopes during the last glacial period".Proceedings of the National Academy of Sciences of the United States of America 116.10(2019). |
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