气候变化领域集成服务门户(CCPortal): Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir

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DOI	10.1007/s00382-021-05827-4
	Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir
	Chen F.; Gagen M.H.; Zhang H.; Chen Y.; Fan Z.; Chen F.
发表日期	2021
ISSN	0930-7575
起始页码	17
结束页码	27
英文摘要	Land-surface temperature changes lead to thermal contrasts between the land and the sea and have significant water cycle impacts particularly within global monsoon regions. Whilst such influence may dominate in the East Asian summer monsoon region, the long-term warm-season temperature dynamics in monsoonal China have not been effectively explored. Here, an annually resolved maximum latewood density (MXD) record from annual tree rings of Shensi fir (A. chensiensis) in the Qinling Mountains (north-central China) provide an East Asian summer monsoon-region relevant 270-year long March-September temperature reconstruction. Our MXD-based temperature reconstruction shows good agreement with phases of observed warming in the 1920s-1950s and 1990s-2000s, a more recent warming hiatus and earlier volcanic-induced cooling phases. Our temperature reconstruction is also significantly correlated with sea surface temperatures in the North Atlantic Ocean and reveals that there is an unstable influence of the Atlantic Multidecadal Oscillation (AMO) on warm season temperature variability in north-central China. Our warm season temperature reconstruction is sensitive to summer monsoonal season moisture variations in north-central China and provides a multi century perspective on the region’s climate which is useful to improving the understanding of monsoonal East Asian climate change and anticipated future extreme drought events in northern China. © 2021, The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature.
英文关键词	Abies chensiensis; East asian summer monsoon; Maximum latewood density; Qinling mountains; Temperature reconstruction; Volcanic eruptions
来源期刊	Climate Dynamics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/183438
作者单位	Yunnan Key Laboratory of International Rivers and Transboundary Eco-Security, Institute of International Rivers and Eco-Security, Yunnan University, Kunming, China; Key Laboratory of Tree-Ring Physical and Chemical Research of China Meteorological Administration/Xinjiang Laboratory of Tree-Ring Ecology, Institute of Desert Meteorology, China Meteorological Administration, Urumqi, China; Epartment of Geography, Swansea University, Singleton Park, Swansea, SA2 8PP, United Kingdom; Key Laboratory of Alpine Ecology, CAS Center for Excellence in Tibetan Plateau Earth Sciences and Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing, 100101, China; Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, China
推荐引用方式 GB/T 7714	Chen F.,Gagen M.H.,Zhang H.,et al. Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir[J],2021.
APA	Chen F.,Gagen M.H.,Zhang H.,Chen Y.,Fan Z.,&Chen F..(2021).Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir.Climate Dynamics.
MLA	Chen F.,et al."Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir".Climate Dynamics (2021).