Tree ring O-18's indication of a shift to a wetter climate since the 1880s in the western Tianshan Mountains of northwestern China

• Published in: Journal of Geophysical Research: Atmospheres
• Main Authors: Xu, Guobao, Liu, Xiaohong, Wu, Guoju, Chen, Tuo, Wang, Wenzhi, Zhang, Qiong, Zhang, Youfu, Zeng, Xiaomin, Qin, Dahe, Sun, Weizhen, Zhang, Xuanwen
• Format: Article in Journal/Newspaper
• Language: English
• Published: AMER GEOPHYSICAL UNION 2015
• Subjects: Tree Ring 18o; Spei; Drought; Pluvials; Regime Shift; China's Western Tianshan Mountains; Science & Technology; Physical Sciences; Southeastern Tibetan Plateau; North-atlantic Oscillation; Drought Severity Index; Isotope Ratios; Delta-o-18 Chronology; Stable-isotopes; Precipitation; Variability; Cellulose; Oxygen; Meteorology & Atmospheric Sciences; Indian; North Atlantic; North Atlantic oscillation
• Online Access: http://ir.ieecas.cn/handle/361006/9263; http://ir.ieecas.cn/handle/361006/9264; https://doi.org/10.1002/2014JD023027

Central Asian droughts have drastically and significantly affected agriculture and water resource management in these arid and semiarid areas. Based on tree ring O-18 from native, dominant Schrenk spruce (Picea schrenkiana Fisch. et Mey.), we developed a 300year (1710-2010) standard precipitation-evaporation index (SPEI) reconstruction from January to August for China's western Tianshan Mountains. The regression model explained 37.6% of the variation in the SPEI reconstruction during the calibration period from 1950 to 2010. Comparison with previous drought reconstructions confirmed the robustness of our reconstruction. The 20th century has been a relatively wet period during the past 300years. The SPEI showed quasi 2, 5, and 10year cycles. Several pluvials and droughts with covariability over large areas were revealed clearly in the reconstruction. The two longest pluvials (lasting for 12years), separated by 50years, appeared in the 1900s and the 1960s. The most severe drought occurred from 1739 to 1761 and from 1886 to 1911 was the wettest period since 1710. Compared to previous investigations of hydroclimatic changes in the western Tianshan Mountains, our reconstruction revealed more low-frequency variability and indicated that climate in the western Tianshan Mountains shifted from dry to wet in 1886. This regime shift was generally consistent with other moisture reconstructions for the northeastern Tibetan Plateau and northern Pakistan and may have resulted from a strengthened westerly circulation. The opposite hydrological trends in the western Tianshan Mountains and southeastern Tibetan Plateau reveal a substantial influence of strengthened westerlies and weakening of the Indian summer monsoon.