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.

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: 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
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2021
Subjects:
Geology
QE1-996.5
Environmental sciences
GE1-350
Antarctic
Antarc*
ice core
Online Access:https://doi.org/10.1038/s43247-021-00304-6
https://doaj.org/article/9bd939c9962f4a0dbe1b6386c48e4487
Description
Summary: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.

Similar Items