DOI | 10.1038/s41467-021-22388-6
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| Millennial scale feedbacks determine the shape and rapidity of glacial termination |
| Barker S.; Knorr G.
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发表日期 | 2021
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ISSN | 2041-1723
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卷号 | 12期号:1 |
英文摘要 | Within the Late Pleistocene, terminations describe the major transitions marking the end of glacial cycles. While it is established that abrupt shifts in the ocean/atmosphere system are a ubiquitous component of deglaciation, significant uncertainties remain concerning their specific role and the likelihood that terminations may be interrupted by large-amplitude abrupt oscillations. In this perspective we address these uncertainties in the light of recent developments in the understanding of glacial terminations as the ultimate interaction between millennial and orbital timescale variability. Innovations in numerical climate simulation and new geologic records allow us to highlight new avenues of research and identify key remaining uncertainties such as sea-level variability. © 2021, The Author(s). |
语种 | 英语
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scopus关键词 | atmosphere-ocean coupling; deglaciation; geological record; glacial-interglacial cycle; last deglaciation; Pleistocene; sea level change; shape; simulation; atmosphere; deglaciation; oscillation; review; sea level; simulation; uncertainty; Upper Pleistocene |
来源期刊 | Nature Communications
(IF:11.878[JCR-2018],13.811[5-Year]) |
文献类型 | 期刊论文
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条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/250714
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作者单位 | School of Earth and Environmental Sciences, Cardiff University, Cardiff, United Kingdom; Alfred Wegener Institute, Bremerhaven, Germany
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推荐引用方式 GB/T 7714 |
Barker S.,Knorr G.. Millennial scale feedbacks determine the shape and rapidity of glacial termination[J],2021,12(1).
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APA |
Barker S.,&Knorr G..(2021).Millennial scale feedbacks determine the shape and rapidity of glacial termination.Nature Communications,12(1).
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MLA |
Barker S.,et al."Millennial scale feedbacks determine the shape and rapidity of glacial termination".Nature Communications 12.1(2021).
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