Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics
Severe cooling at high northern latitudes, which marked the onset of Heinrich Stadial 4, was synchronous with changes in tropical monsoon systems and preceded Antarctic warming by around 300 years, according to a compilation of speleothem and ice core records.
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Nature Portfolio
2021
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oai:doaj.org-article:9bd939c9962f4a0dbe1b6386c48e44872021-11-14T12:12:53ZOnset and termination of Heinrich Stadial 4 and the underlying climate dynamics10.1038/s43247-021-00304-62662-4435https://doaj.org/article/9bd939c9962f4a0dbe1b6386c48e44872021-11-01T00:00:00Zhttps://doi.org/10.1038/s43247-021-00304-6https://doaj.org/toc/2662-4435Severe cooling at high northern latitudes, which marked the onset of Heinrich Stadial 4, was synchronous with changes in tropical monsoon systems and preceded Antarctic warming by around 300 years, according to a compilation of speleothem and ice core records.Hai ChengYao XuXiyu DongJingyao ZhaoHanying LiJonathan BakerAshish SinhaChristoph SpötlHaiwei ZhangWenjing DuBaoyun ZongXue JiaGayatri KathayatDianbing LiuYanjun CaiXianfeng WangNicolás M. StrikisFrancisco W. CruzAugusto S. AulerAnil K. GuptaRaj Kumar SinghSonu JaglanSom DuttZhengyu LiuR. Lawrence EdwardsNature PortfolioarticleGeologyQE1-996.5Environmental sciencesGE1-350ENCommunications Earth & Environment, Vol 2, Iss 1, Pp 1-11 (2021) |
| institution |
DOAJ |
| collection |
DOAJ |
| language |
EN |
| topic |
Geology QE1-996.5 Environmental sciences GE1-350 |
| spellingShingle |
Geology QE1-996.5 Environmental sciences GE1-350 Hai Cheng Yao Xu Xiyu Dong Jingyao Zhao Hanying Li Jonathan Baker Ashish Sinha Christoph Spötl Haiwei Zhang Wenjing Du Baoyun Zong Xue Jia Gayatri Kathayat Dianbing Liu Yanjun Cai Xianfeng Wang Nicolás M. Strikis Francisco W. Cruz Augusto S. Auler Anil K. Gupta Raj Kumar Singh Sonu Jaglan Som Dutt Zhengyu Liu R. Lawrence Edwards Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics |
| description |
Severe cooling at high northern latitudes, which marked the onset of Heinrich Stadial 4, was synchronous with changes in tropical monsoon systems and preceded Antarctic warming by around 300 years, according to a compilation of speleothem and ice core records. |
| format |
article |
| author |
Hai Cheng Yao Xu Xiyu Dong Jingyao Zhao Hanying Li Jonathan Baker Ashish Sinha Christoph Spötl Haiwei Zhang Wenjing Du Baoyun Zong Xue Jia Gayatri Kathayat Dianbing Liu Yanjun Cai Xianfeng Wang Nicolás M. Strikis Francisco W. Cruz Augusto S. Auler Anil K. Gupta Raj Kumar Singh Sonu Jaglan Som Dutt Zhengyu Liu R. Lawrence Edwards |
| author_facet |
Hai Cheng Yao Xu Xiyu Dong Jingyao Zhao Hanying Li Jonathan Baker Ashish Sinha Christoph Spötl Haiwei Zhang Wenjing Du Baoyun Zong Xue Jia Gayatri Kathayat Dianbing Liu Yanjun Cai Xianfeng Wang Nicolás M. Strikis Francisco W. Cruz Augusto S. Auler Anil K. Gupta Raj Kumar Singh Sonu Jaglan Som Dutt Zhengyu Liu R. Lawrence Edwards |
| author_sort |
Hai Cheng |
| title |
Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics |
| title_short |
Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics |
| title_full |
Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics |
| title_fullStr |
Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics |
| title_full_unstemmed |
Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics |
| title_sort |
onset and termination of heinrich stadial 4 and the underlying climate dynamics |
| publisher |
Nature Portfolio |
| publishDate |
2021 |
| url |
https://doaj.org/article/9bd939c9962f4a0dbe1b6386c48e4487 |
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