Arid
DOI10.3390/f10030223
The Radial Growth of Schrenk Spruce (Picea schrenkiana Fisch. et Mey.) Records the Hydroclimatic Changes in the Chu River Basin over the Past 175 Years
Zhang, Ruibo1,2,3; Ermenbaev, Bakytbek4; Zhang, Tongwen1; Ali, Mamtimin1; Qin, Li1; Satylkanov, Rysbek4
通讯作者Zhang, Ruibo
来源期刊FORESTS
ISSN1999-4907
出版年2019
卷号10期号:3
英文摘要The Chu River is one of the most important rivers in arid Central Asia. Its discharge is affected by climate change. Here, we establish a tree-ring chronology for the upper Chu River Basin and analyze the relationships between radial growth, climate, and discharge. The results show that the radial growth of Schrenk spruce (Picea schrenkiana Fisch. et Mey.) is controlled by moisture. We also reconstruct a 175-year standardized precipitation-evapotranspiration index (SPEI) for the Chu River Basin. A comparison of the reconstructed and observed indices reveal that 39.5% of the variance occurred during the calibration period of 1952-2014. The SPEI reconstruction and discharge variability of the Chu River show consistent long-term change. They also show that the Chu River Basin became increasingly dry between the 1840s and the 1960s, with a significant drought during the 1970s. A long and rapid wetting period occurred between the 1970s and the 2000s, and was followed by increasing drought since 2004. The change in the SPEI in the Chu River Basin is consistent with records of long-term precipitation, SPEI and Palmer Drought Severity Indices (PDSI) in other proximate regions of the western Tianshan Mountains. The hydroclimatic change of the Chu River Basin may be associated with westerly wind. This study is helpful for disaster prevention and water resource management in arid central Asia.
英文关键词tree rings Schrenk spruce (Picea schrenkiana Fisch et Mey ) hydroclimatology Chu River Tianshan Mountains climate change Central Asia
类型Article
语种英语
国家Peoples R China ; Kyrgyzstan
开放获取类型gold, Green Submitted
收录类别SCI-E
WOS记录号WOS:000464453900003
WOS关键词CENTRAL-ASIA ; TIANSHAN MOUNTAINS ; CLIMATE-CHANGE ; TREE-RINGS ; DROUGHT ; RECONSTRUCTION ; CHINA ; VARIABILITY ; LINKAGES ; MOISTURE
WOS类目Forestry
WOS研究方向Forestry
来源机构中国科学院大气物理研究所 ; 南京信息工程大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/215686
作者单位1.China Meteorol Adm, Inst Desert Meteorol, Key Lab Tree Ring Phys & Chem Res, Key Lab Tree Ring Ecol Xinjiang Uigur Autonomous, Urumqi 830002, Peoples R China;
2.Chinese Acad Sci, Inst Atmospher Phys, Climate Change Res Ctr, Beijing 100029, Peoples R China;
3.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Joint Int Res Lab Climate & Environm Change, Key Lab Meteorol Disaster,Minist Educ, Nanjing 210044, Jiangsu, Peoples R China;
4.Natl Acad Sci Kyrgyz Republ, Inst Water Problem & Hydropower, Tien Shan Sci Ctr, Bishkek 720033, Kyrgyzstan
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Zhang, Ruibo,Ermenbaev, Bakytbek,Zhang, Tongwen,et al. The Radial Growth of Schrenk Spruce (Picea schrenkiana Fisch. et Mey.) Records the Hydroclimatic Changes in the Chu River Basin over the Past 175 Years[J]. 中国科学院大气物理研究所, 南京信息工程大学,2019,10(3).
APA Zhang, Ruibo,Ermenbaev, Bakytbek,Zhang, Tongwen,Ali, Mamtimin,Qin, Li,&Satylkanov, Rysbek.(2019).The Radial Growth of Schrenk Spruce (Picea schrenkiana Fisch. et Mey.) Records the Hydroclimatic Changes in the Chu River Basin over the Past 175 Years.FORESTS,10(3).
MLA Zhang, Ruibo,et al."The Radial Growth of Schrenk Spruce (Picea schrenkiana Fisch. et Mey.) Records the Hydroclimatic Changes in the Chu River Basin over the Past 175 Years".FORESTS 10.3(2019).
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