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DOI | 10.1073/pnas.1104772108 |
Ice-shelf collapse from subsurface warming as a trigger for Heinrich events | |
Marcott S.A.; Clark P.U.; Padman L.; Klinkhammer G.P.; Springer S.R.; Liu Z.; Otto-Bliesner B.L.; Carlson A.E.; Ungerer A.; Padman J.; He F.; Cheng J.; Schmittner A. | |
发表日期 | 2011 |
ISSN | 0027-8424 |
起始页码 | 13415 |
结束页码 | 13419 |
卷号 | 108期号:33 |
英文摘要 | Episodic iceberg-discharge events from the Hudson Strait Ice Stream (HSIS) of the Laurentide Ice Sheet, referred to as Heinrich events, are commonly attributed to internal ice-sheet instabilities, but their systematic occurrence at the culmination of a large reduction in the Atlantic meridional overturning circulation (AMOC) indicates a climate control. We report Mg/Ca data on benthic foraminifera from an intermediate-depth site in the northwest Atlantic and results from a climate-model simulation that reveal basin-wide subsurface warming at the same time as large reductions in the AMOC, with temperature increasing by approximately 2°C over a 1-2 kyr interval prior to a Heinrich event. In simulations with an ocean model coupled to a thermodynamically active ice shelf, the increase in subsurface temperature increases basal melt rate under an ice shelf fronting the HSIS by a factor of approximately 6. By analogy with recent observations in Antarctica, the resulting ice-shelf loss and attendant HSIS acceleration would produce a Heinrich event. |
英文关键词 | Abrupt climate change; Paleoceanography; Paleoclimatology |
语种 | 英语 |
scopus关键词 | calcium; magnesium; Antarctica; article; benthic foraminifera; climate; heinrich event; Holocene; ice shelf; nonhuman; North Atlantic deep water; priority journal; simulation; temperature measurement; thermodynamics; warming; Calcium; Climate; Foraminifera; Greenhouse Effect; Ice Cover; Magnesium; Oceans and Seas; Temperature; Water Movements; Foraminifera |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/159143 |
作者单位 | Marcott, S.A., Department of Geosciences, Oregon State University, Corvallis, OR 97331, United States; Clark, P.U., Department of Geosciences, Oregon State University, Corvallis, OR 97331, United States; Padman, L., Earth and Space Research, 3350 SW Cascade Avenue, Corvallis, OR 97333, United States; Klinkhammer, G.P., College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, United States; Springer, S.R., Earth and Space Research, 2101 Fourth Avenue, Seattle, WA 98121, United States; Liu, Z., Center for Climatic Research, Department of Atmospheric and Oceanic Sciences, University of Wisconsin, Madison, WI 53706, United States; Otto-Bliesner, B.L., Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO 80307, United States; Carlson, A.E., Center for Climatic Research, Department of Atmospheric and Oceanic Sciences, University of Wisconsin, Madison, WI 53706, United States, Department of Geoscience, University of Wisconsin, Madison, WI 5... |
推荐引用方式 GB/T 7714 | Marcott S.A.,Clark P.U.,Padman L.,et al. Ice-shelf collapse from subsurface warming as a trigger for Heinrich events[J],2011,108(33). |
APA | Marcott S.A..,Clark P.U..,Padman L..,Klinkhammer G.P..,Springer S.R..,...&Schmittner A..(2011).Ice-shelf collapse from subsurface warming as a trigger for Heinrich events.Proceedings of the National Academy of Sciences of the United States of America,108(33). |
MLA | Marcott S.A.,et al."Ice-shelf collapse from subsurface warming as a trigger for Heinrich events".Proceedings of the National Academy of Sciences of the United States of America 108.33(2011). |
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