Possible obliquity-forced warmth in southern Asia during the last glacial stage

[Display omitted] Orbital-scale global climatic changes during the late Quaternary are dominated by high-latitude influenced ~100,000-year global ice-age cycles and monsoon influenced ~23,000-year low-latitude hydroclimate variations. However, the shortage of highly-resolved land temperature records...

Full description

Saved in:
Bibliographic Details
Published inScience bulletin Vol. 66; no. 11; pp. 1136 - 1145
Main Authors Zhao, Cheng, Rohling, Eelco J., Liu, Zhengyu, Yang, Xiaoqiang, Zhang, Enlou, Cheng, Jun, Liu, Zhonghui, An, Zhisheng, Yang, Xiangdong, Feng, Xiaoping, Sun, Xiaoshuang, Zhang, Can, Yan, Tianlong, Long, Hao, Yan, Hong, Yu, Zicheng, Liu, Weiguo, Yu, Shi-Yong, Shen, Ji
Format Journal Article
LanguageEnglish
Published Netherlands Elsevier B.V 15.06.2021
Subjects
Online AccessGet full text

Cover

Loading…