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DOI10.1038/s41467-021-22388-6
Millennial scale feedbacks determine the shape and rapidity of glacial termination
Barker S.; Knorr G.
发表日期2021
ISSN2041-1723
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
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
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/250714
作者单位School of Earth and Environmental Sciences, Cardiff University, Cardiff, United Kingdom; Alfred Wegener Institute, Bremerhaven, Germany
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Barker S.,Knorr G.. Millennial scale feedbacks determine the shape and rapidity of glacial termination[J],2021,12(1).
APA Barker S.,&Knorr G..(2021).Millennial scale feedbacks determine the shape and rapidity of glacial termination.Nature Communications,12(1).
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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