Late Holocene hydroclimatic variation in central Asia and its response to mid-latitude Westerlies and solar irradiance

doi:10.1016/j.quascirev.2020.106330

IEECAS OpenIR

	Late Holocene hydroclimatic variation in central Asia and its response to mid-latitude Westerlies and solar irradiance
	Lan, Jianghu 1,2; Zhang, Jin 3; Cheng, Peng 1,2; Ma, Xiaolin 1,2; Ai, Li 1,2; Chawchai, Sakonvan 4; Zhou, Kang'en 1,5; Wang, Tianli 1,5; Yu, Keke 6; Sheng, Enguo 7; Kang, Shugang 1,2; Zang, Jingjie 1; Yan, Dongna 1,5; Wang, Yaqin 1; Tan, Liangcheng 1,2,8; Xu, Hai 2,3
通讯作者	Lan, Jianghu(lanjh@ieecas.cn) ; Zhang, Jin(zhangjin968@tju.edu.cn)
	2020-06-15
发表期刊	QUATERNARY SCIENCE REVIEWS
ISSN	0277-3791
卷号	238 页码:14
摘要	Hydroclimatic variations in central Asia are widely recognized to be tele-connected with the North Atlantic climate via the mid-latitude Westerlies. However, the long-term hydroclimatic variation and its response to North Atlantic climate changes are not fully understood. Here we report multi-decadal and centennial hydroclimatic variations in central Asia during the late Holocene using high-resolution oxygen and carbon isotopes of bulk carbonate from a remote hydrologically closed alpine lake in Tianshan Mountains, northwestern China. The hydroclimatic variations inferred from the covariance between delta O-18(carb) and delta C-13(carb) and published multi-proxy in the Lake Sayram together agree well with the records from the central Asia, showing enhanced effective moisture at the intervals of 4000-3780, 3590-3210, 2800-2160, 1700-1370 and 890-280 cal yr BP during the negative phase of North Atlantic Oscillation (NAO). Comparison with European hydroclimatic changes on centennial scale, our records not only provide valuable insight into the hydroclimatic variations in central Asia, but also indicate all broadly contemporaneous changes with that of southern Europe whereas antiphase with that of northern Europe. We then conclude that the observed antiphase hydroclimatic pattern between northern Europe and southern Europe-central Asia on centennial time scale during the late Holocene were persistently controlled by the north-south migration of mid-latitude Westerlies and changes of NAO phase in response to solar irradiance forcing. However, further research is necessary to fully disentangle the natural and anthropogenic forcing mechanisms for enhanced effect moisture and/or precipitation in central Asia. (C) 2020 Elsevier Ltd. All rights reserved.
关键词	Hydroclimatic variation Central Asia Late holocene North Atlantic oscillation Mid-latitude Westerlies Solar irradiance
DOI	10.1016/j.quascirev.2020.106330
关键词[WOS]	NORTH-ATLANTIC OSCILLATION ; RADIOCARBON AGE CALIBRATION ; LAKE-LEVEL FLUCTUATIONS ; INTERTROPICAL CONVERGENCE ZONE ; MEDIEVAL WARM PERIOD ; LAST 4000 YEARS ; CLIMATE-CHANGE ; ICE-AGE ; SEDIMENT RECORD ; HUMAN-IMPACT
收录类别	SCI ; SCI
语种	英语
资助项目	2nd Tibetan Plateau Scientific Expedition and Research[2019QZKK0101] ; National Natural Science Foundation of China[41991253] ; National Natural Science Foundation of China[41672169] ; National Natural Science Foundation of China[41701032] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB40010300] ; National Natural Science Foundation of China-Israel Science Foundation research program[41761144070] ; Youth Innovation Promotion Association of Chinese Academy of Sciences[2012295] ; Special Exchange Program of Chinese Academy of Sciences[E029020147] ; National Social Science Foundation of China[18ZDA172]
WOS研究方向	Physical Geography ; Geology
项目资助者	2nd Tibetan Plateau Scientific Expedition and Research ; National Natural Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China-Israel Science Foundation research program ; Youth Innovation Promotion Association of Chinese Academy of Sciences ; Special Exchange Program of Chinese Academy of Sciences ; National Social Science Foundation of China
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000537559500008
出版者	PERGAMON-ELSEVIER SCIENCE LTD
引用统计
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/14864
通讯作者	Lan, Jianghu; Zhang, Jin
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quatemary Geol, Xian 710061, Peoples R China 2.Chinese Acad Sci, Ctr Excellence Quatemary Sci & Global Change, Xian 710061, Peoples R China 3.Tianjin Univ, Inst Surface Earth Syst Sci, Tianjin 300072, Peoples R China 4.Chulalongkorn Univ, Fac Sci, Dept Geol, Bangkok 10330, Thailand 5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 6.Baoji Univ Arts & Sci, Key Lab Disaster Monitoring & Mech Simulating Sha, Baoji 721013, Shaanxi, Peoples R China 7.Zunyi Normal Univ, Coll Resources & Environm, Zunyi 563006, Guizhou, Peoples R China 8.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China
推荐引用方式 GB/T 7714	Lan, Jianghu,Zhang, Jin,Cheng, Peng,et al. Late Holocene hydroclimatic variation in central Asia and its response to mid-latitude Westerlies and solar irradiance[J]. QUATERNARY SCIENCE REVIEWS,2020,238:14.
APA	Lan, Jianghu.,Zhang, Jin.,Cheng, Peng.,Ma, Xiaolin.,Ai, Li.,...&Xu, Hai.(2020).Late Holocene hydroclimatic variation in central Asia and its response to mid-latitude Westerlies and solar irradiance.QUATERNARY SCIENCE REVIEWS,238,14.
MLA	Lan, Jianghu,et al."Late Holocene hydroclimatic variation in central Asia and its response to mid-latitude Westerlies and solar irradiance".QUATERNARY SCIENCE REVIEWS 238(2020):14.