Position and orientation of the westerly jet determined Holocene rainfall patterns in China
The basic mechanisms behind the East Asian Summer Monsoon remain poorly understood. Using proxy-based reconstructions and simulations, here the authors show that changes in the orientation and position of the westerly jet stream resulted in regionally asynchronous Holocene precipitation maxima.
Guardado en:
Autores principales: | Ulrike Herzschuh, Xianyong Cao, Thomas Laepple, Anne Dallmeyer, Richard J. Telford, Jian Ni, Fahu Chen, Zhaochen Kong, Guangxiu Liu, Kam-Biu Liu, Xingqi Liu, Martina Stebich, Lingyu Tang, Fang Tian, Yongbo Wang, Juliane Wischnewski, Qinghai Xu, Shun Yan, Zhenjing Yang, Ge Yu, Yun Zhang, Yan Zhao, Zhuo Zheng |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
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Materias: | |
Acceso en línea: | https://doaj.org/article/5c7224d965764bf4b29fedb5945e7c67 |
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