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DOI10.1038/s41558-020-0897-7
Weakening Atlantic overturning circulation causes South Atlantic salinity pile-up
Zhu C.; Liu Z.
发表日期2020
ISSN1758-678X
起始页码998
结束页码1003
卷号10期号:11
英文摘要The Atlantic Meridional Overturning Circulation (AMOC) is an active component of the Earth’s climate system1 and its response to global warming is of critical importance to society. Climate models have shown an AMOC slowdown under anthropogenic warming since the industrial revolution2–4, but this slowdown has been difficult to detect in the short observational record5–10 because of substantial interdecadal climate variability. This has led to the indirect detection of the slowdown from longer-term fingerprints11–14 such as the subpolar North Atlantic ‘warming hole’11. However, these fingerprints, which exhibit some uncertainties15, are all local indicators of AMOC slowdown around the subpolar North Atlantic. Here we show observational and modelling evidence of a remote indicator of AMOC slowdown outside the North Atlantic. Under global warming, the weakening AMOC reduces the salinity divergence and then leads to a ‘salinity pile-up’ remotely in the South Atlantic. This evidence is consistent with the AMOC slowdown under anthropogenic warming and, furthermore, suggests that this weakening has likely occurred all the way into the South Atlantic. © 2020, The Author(s), under exclusive licence to Springer Nature Limited.
语种英语
来源期刊Nature Climate Change
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/171648
作者单位Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao, China; Open Studio for Ocean-Climate-Isotope Modeling, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China; Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China; College of Geography Science, Nanjing Normal University, Nanjing, China; Atmospheric Science Program, Department of Geography, Ohio State University, Columbus, OH, United States
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Zhu C.,Liu Z.. Weakening Atlantic overturning circulation causes South Atlantic salinity pile-up[J],2020,10(11).
APA Zhu C.,&Liu Z..(2020).Weakening Atlantic overturning circulation causes South Atlantic salinity pile-up.Nature Climate Change,10(11).
MLA Zhu C.,et al."Weakening Atlantic overturning circulation causes South Atlantic salinity pile-up".Nature Climate Change 10.11(2020).
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