Tracking westerly wind directions over Europe since the middle Holocene

The variability of the northern westerlies has been considered as one of the key elements for modern and past climate evolution. Their multiscale behavior and underlying control mechanisms, however, are incompletely understood, owing to the complex dynamics of Atlantic sea-level pressures. Here, we...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Hu, Hsun-Ming, Trouet, Valerie, Spötl, Christoph, Tsai, Hsien-Chen, Chien, Wei-Yi, Sung, Wen-Hui, Michel, Véronique, Yu, Jin-Yi, Valensi, Patricia, Jiang, Xiuyang, Duan, Fucai, Wang, Yongjin, Mii, Horng-Sheng, Chou, Yu-Min, Lone, Mahjoor Ahmad, Wu, Chung-Che, Starnini, Elisabetta, Zunino, Marta, Watanabe, Takaaki K, Watanabe, Tsuyoshi, Hsu, Huang-Hsiung, Moore, G W K, Zanchetta, Giovanni, Pérez-Mejías, Carlos, Lee, Shih-Yu, Shen, Chuan-Chou
Other Authors: Pérez-Mejías, Carlo
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/11568/1161326
https://doi.org/10.1038/s41467-022-34952-9
Description
Summary:The variability of the northern westerlies has been considered as one of the key elements for modern and past climate evolution. Their multiscale behavior and underlying control mechanisms, however, are incompletely understood, owing to the complex dynamics of Atlantic sea-level pressures. Here, we present a multi-annually resolved record of the westerly drift over the past 6,500 years from northern Italy. In combination with more than 20 other westerly-sensitive records, our results depict the non-stationary westerly-affected regions over mainland Europe on multi-decadal to multi-centennial time scales, showing that the direction of the westerlies has changed with respect to the migrations of the North Atlantic centers of action since the middle Holocene. Our findings suggest the crucial role of the migrations of the North Atlantic dipole in modulating the westerly-affected domain over Europe, possibly modulated by Atlantic Ocean variability.