Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems

Melting of permafrost and growth of peatland in southwest Siberia after the Younger Dryas was likely linked to reorganization of westerly wind systems and a weakened Siberian High, according to multiproxy speleothem data from the Altai mountains.

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Autores principales: Ting-Yong Li, Jonathan L. Baker, Tao Wang, Jian Zhang, Yao Wu, Hong-Chun Li, Tatiana Blyakharchuk, Tsai-Luen Yu, Chuan-Chou Shen, Hai Cheng, Xing-Gong Kong, Wen-Li Xie, R. Lawrence Edwards
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Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/29f7ee1b998a4739a8b21c443b70ad57
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spelling oai:doaj.org-article:29f7ee1b998a4739a8b21c443b70ad572021-12-02T17:18:19ZEarly Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems10.1038/s43247-021-00238-z2662-4435https://doaj.org/article/29f7ee1b998a4739a8b21c443b70ad572021-09-01T00:00:00Zhttps://doi.org/10.1038/s43247-021-00238-zhttps://doaj.org/toc/2662-4435Melting of permafrost and growth of peatland in southwest Siberia after the Younger Dryas was likely linked to reorganization of westerly wind systems and a weakened Siberian High, according to multiproxy speleothem data from the Altai mountains.Ting-Yong LiJonathan L. BakerTao WangJian ZhangYao WuHong-Chun LiTatiana BlyakharchukTsai-Luen YuChuan-Chou ShenHai ChengXing-Gong KongWen-Li XieR. Lawrence EdwardsNature PortfolioarticleGeologyQE1-996.5Environmental sciencesGE1-350ENCommunications Earth & Environment, Vol 2, Iss 1, Pp 1-11 (2021)
institution DOAJ
collection DOAJ
language EN
topic Geology
QE1-996.5
Environmental sciences
GE1-350
spellingShingle Geology
QE1-996.5
Environmental sciences
GE1-350
Ting-Yong Li
Jonathan L. Baker
Tao Wang
Jian Zhang
Yao Wu
Hong-Chun Li
Tatiana Blyakharchuk
Tsai-Luen Yu
Chuan-Chou Shen
Hai Cheng
Xing-Gong Kong
Wen-Li Xie
R. Lawrence Edwards
Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems
description Melting of permafrost and growth of peatland in southwest Siberia after the Younger Dryas was likely linked to reorganization of westerly wind systems and a weakened Siberian High, according to multiproxy speleothem data from the Altai mountains.
format article
author Ting-Yong Li
Jonathan L. Baker
Tao Wang
Jian Zhang
Yao Wu
Hong-Chun Li
Tatiana Blyakharchuk
Tsai-Luen Yu
Chuan-Chou Shen
Hai Cheng
Xing-Gong Kong
Wen-Li Xie
R. Lawrence Edwards
author_facet Ting-Yong Li
Jonathan L. Baker
Tao Wang
Jian Zhang
Yao Wu
Hong-Chun Li
Tatiana Blyakharchuk
Tsai-Luen Yu
Chuan-Chou Shen
Hai Cheng
Xing-Gong Kong
Wen-Li Xie
R. Lawrence Edwards
author_sort Ting-Yong Li
title Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems
title_short Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems
title_full Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems
title_fullStr Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems
title_full_unstemmed Early Holocene permafrost retreat in West Siberia amplified by reorganization of westerly wind systems
title_sort early holocene permafrost retreat in west siberia amplified by reorganization of westerly wind systems
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/29f7ee1b998a4739a8b21c443b70ad57
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