학술논문

Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics
Document Type
article
Source
Communications Earth & Environment, Vol 2, Iss 1, Pp 1-11 (2021)
Subject
Geology
QE1-996.5
Environmental sciences
GE1-350
Language
English
ISSN
2662-4435
Abstract
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.