Extreme precipitation stable isotopic compositions reveal unexpected summer monsoon incursions in the Qilian Mountains

被引:10
作者
Zhao, Liangju [1 ]
Dong, Xiying [1 ]
Liu, Xiaohong [2 ]
Wang, Ninglian [1 ]
Eastoe, Christopher J. [3 ]
Wei, Na [4 ]
Xie, Cong [1 ]
Liu, Hang [1 ]
Han, Chuntan [5 ]
Hua, Ting [1 ]
Wang, Lixin [6 ]
机构
[1] Northwest Univ, Coll Urban & Environm Sci, Shaanxi Key Lab Earth Surface & Environm Carrying, Xian 710127, Peoples R China
[2] Shaanxi Normal Univ, Sch Geog & Tourism, Xian 710119, Peoples R China
[3] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
[4] Climate Ctr Shaanxi Prov, Xian 710049, Peoples R China
[5] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Ecol Safety & Sustainable Dev Arid Lands, Lanzhou 730000, Peoples R China
[6] IUPUI, Dept Earth Sci, Indianapolis, IN 46202 USA
基金
中国国家自然科学基金;
关键词
Atmospheric circulation; Moisture origin; Monsoons; Qilian Mountains; Stable isotopes; Westerly circulation; ICE CORE EVIDENCE; CLIMATE-CHANGE; HEIHE RIVER; ATMOSPHERIC MOISTURE; TIBETAN PLATEAU; ASIAN MONSOON; RESIDENCE TIME; TEMPERATURE; DELTA-O-18; ORIGIN;
D O I
10.1016/j.scitotenv.2023.165743
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Isotope composition and moisture sources of precipitation are important for understanding water cycles and reconstructing paleoclimate. Based on 15-years' precipitation stable Isotope composition (818O and 82H) from four stations of the Qilian Mountains, we found unique 818O and 82H features associated with the incursion of the summer monsoon over the Qilian Mountains, northwestern China. In 12 of the 15 years, similar seasonal variations of 818O and 82H confirmed a dominant source of moisture from Westerly circulation, and higher intercepts of the local meteoric water line (LMWL) indicated strong recycling of continental moisture. However, in August 2016 and 2018, extremely low slopes and intercepts of the LMWL, and more negative 818O and 82H revealed substantial contributions of the Asian summer monsoon to precipitation of the Qilian Mountains, with extremely heavy precipitation in August 2016. The column moisture flux, land-sea thermal contrast, correlations of precipitation 818O with East Asian Summer Monsoon Index and Westerlies Index, HYSPLIT modeling results and precipitation 818O along backward trajectories confirmed incursions of the summer monsoon in August 2016 and 2018. Our redefining of the boundary of the summer monsoon region confirmed the summer monsoon incursion zone can extend to the west of longitude 96 degrees E and north of latitude 40 degrees N in strong monsoon years, corresponding to boundaries of monsoon incursions in the mid-Holocene. Temperature correlated with precipitation 818O at monthly and shorter time scales, but not for whole seasons or at yearly scale, revealing that summer monsoon incursions are therefore more likely than changing temperature to explain the multi-year cycles in the Qilian Mountains ice archives. Continent-scale shifts in atmospheric circulation strongly influence water resources in the Qilian mountains, and may change in frequency as climate warms. This study therefore has important implications for understanding water resources in the Qilian mountains in the past and into the future.
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页数:16
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