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

文献类型：期刊论文

作者Zhang, Tongwen2,3,4; Liu, Yu1; Zhang, Ruibo2,3,4; Yu, Shulong2,3,4; Fan, Yuting2,3,4; Shang, Huaming2,3,4; Jiang, Shengxia2,3,4; Qin, Li2,3,4; Zhang, Heli2,3,4
刊名DENDROCHRONOLOGIA
出版日期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
DOI10.1016/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(1803, 1804, 1836, 1923, and 1959) and six drought events (1894, 1916, 1917, 1918, 1931, and 1944) that were noted in historical documents.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.
WOS关键词TIEN-SHAN MOUNTAINS ; LATEWOOD-DENSITY CHRONOLOGIES ; PRECIPITATION RECONSTRUCTION ; TEMPERATURE RECONSTRUCTION ; INNER-MONGOLIA ; SOLAR-ACTIVITY ; CLIMATE-CHANGE ; ANNUAL RUNOFF ; DROUGHT ; CHINA
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研究方向Forestry ; Physical Geography
语种英语
WOS记录号WOS:000537249900006
出版者ELSEVIER GMBH
资助机构National Natural Science Foundation of China ; Key Laboratory Opening Subject of Xinjiang Uigur Autonomous Region ; Edanz Group China
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.Chinese Acad Sci, Inst Earth Environm, Xian 710061, Peoples R China
2.China Meteorol Adm, Inst Desert Meteorol, Urumqi 830002, Peoples R China
3.China Meteorol Adm, Key Lab Tree Ring Phys & Chem Res, Urumqi 830002, Peoples R China
4.Key Lab Tree Ring Ecol Uigur Autonomous Reg, 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.

入库方式： OAI收割

来源：地球环境研究所

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