Tree-ring width based streamflow reconstruction for the Kaidu River originating from the central Tianshan Mountains since AD 1700

doi:10.1016/j.dendro.2020.125700

	Tree-ring width based streamflow reconstruction for the Kaidu River originating from the central Tianshan Mountains since AD 1700
	Zhang, Tongwen 1,2,4; Liu, Yu 3; Zhang, Ruibo 1,2,4; Yu, Shulong 1,2,4; Fan, Yuting 1,2,4; Shang, Huaming 1,2,4; Jiang, Shengxia 1,2,4; Qin, Li 1,2,4; Zhang, Heli 1,2,4
刊名	DENDROCHRONOLOGIA
	2020-06-01
卷号	61 页码:13
关键词	Picea schrenkiana tree-ring width climatic responses streamflow reconstruction Kaidu River
ISSN号	1125-7865
DOI	10.1016/j.dendro.2020.125700
通讯作者	Zhang, Tongwen(zhangtw@idm.cn)
英文摘要	In this study, a 310-year pSeptember-August record of streamflow (where p denotes a month from the previous year) for the Kaidu River was reconstructed based on tree-ring-width from 137 Schrenk spruces (Picea schrenkiana). Spatial correlation showed that this streamflow reconstruction contains local hydroclimatic signals that approximately overlap the Kaidu River watershed. A comparison between the streamflow reconstruction for the Kaidu River and five tree-ring-based hydrological reconstructions for the surrounding areas revealed similar variations in the low-frequency domain. The results of comparison analyses between this reconstruction and other hydrological reconstructions indicated that the hydrological characteristics of the Kaidu River in the 1910s (the driest decade for the Kaidu River in the last 310 years), and the increasing trend of streamflow that began in the 1980s, might have occurred in other areas of the Tianshan Mountains and covered an even larger area. Furthermore, the highest and lowest values of this reconstructed streamflow series capture five flood or snowfall events (1803, 1804, 1836, 1923, and 1959) and six drought events (1894, 1916, 1917, 1918, 1931, and 1944) that were noted in historical documents. The 10.8- and 3.5-5.4-year cycles of this reconstruction coincided with the observed data and other tree-ring based hydrometeorological reconstructions, and revealed the possible influences of solar activity and the atmosphere-ocean system.
资助项目	National Natural Science Foundation of China[U1803245] ; National Natural Science Foundation of China[41975095] ; Key Laboratory Opening Subject of Xinjiang Uigur Autonomous Region[2018D04028] ; Key Laboratory Opening Subject of Xinjiang Uigur Autonomous Region[2016D03005] ; Edanz Group China
WOS关键词	TIEN-SHAN MOUNTAINS ; LATEWOOD-DENSITY CHRONOLOGIES ; PRECIPITATION RECONSTRUCTION ; TEMPERATURE RECONSTRUCTION ; INNER-MONGOLIA ; SOLAR-ACTIVITY ; CLIMATE-CHANGE ; ANNUAL RUNOFF ; DROUGHT ; CHINA
WOS研究方向	Forestry ; Physical Geography
语种	英语
出版者	ELSEVIER GMBH
WOS记录号	WOS:000537249900006
资助机构	National Natural Science Foundation of China ; Key Laboratory Opening Subject of Xinjiang Uigur Autonomous Region ; Edanz Group China
内容类型	期刊论文
源URL	[http://ir.ieecas.cn/handle/361006/14888]
专题	地球环境研究所_现代环境研究室
通讯作者	Zhang, Tongwen
作者单位	1.Key Lab Tree Ring Ecol Uigur Autonomous Reg, Urumqi 830002, Peoples R China 2.China Meteorol Adm, Key Lab Tree Ring Phys & Chem Res, Urumqi 830002, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, Xian 710061, Peoples R China 4.China Meteorol Adm, Inst Desert Meteorol, Urumqi 830002, Peoples R China
推荐引用方式 GB/T 7714	Zhang, Tongwen,Liu, Yu,Zhang, Ruibo,et al. Tree-ring width based streamflow reconstruction for the Kaidu River originating from the central Tianshan Mountains since AD 1700[J]. DENDROCHRONOLOGIA,2020,61:13.
APA	Zhang, Tongwen.,Liu, Yu.,Zhang, Ruibo.,Yu, Shulong.,Fan, Yuting.,...&Zhang, Heli.(2020).Tree-ring width based streamflow reconstruction for the Kaidu River originating from the central Tianshan Mountains since AD 1700.DENDROCHRONOLOGIA,61,13.
MLA	Zhang, Tongwen,et al."Tree-ring width based streamflow reconstruction for the Kaidu River originating from the central Tianshan Mountains since AD 1700".DENDROCHRONOLOGIA 61(2020):13.