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.
引用
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页数:16
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共 89 条
  • [1] Stable isotope evidence for moisture sources in the Asian summer monsoon under present and past climate regimes -: art. no. L08203
    Aggarwal, PK
    Fröhlich, K
    Kulkarni, KM
    Gourcy, LL
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (08) : L082031 - 4
  • [2] Isotopic composition and origin of the precipitation in Northern Chile
    Aravena, R
    Suzuki, O
    Peña, H
    Pollastri, A
    Fuenzalida, H
    Grilli, A
    [J]. APPLIED GEOCHEMISTRY, 1999, 14 (04) : 411 - 422
  • [3] Isotopic variation in Indian Monsoon precipitation: Records from Bombay and New Delhi
    Bhattacharya, SK
    Froehlich, K
    Aggarwal, PK
    Kulkarni, KM
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (24) : ASC11 - 1
  • [4] Atmospheric circulation controls on precipitation isotope-climate relations in western Canada
    Birks, S. J.
    Edwards, T. W. D.
    [J]. TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2009, 61 (03): : 566 - 576
  • [5] Vegetation Control in the Long-Term Self-Stabilization of the Liangzhou Oasis of the Upper Shiyang River Watershed of West-Central Gansu, Northwest China
    Bourque, Charles P. -A.
    Hassan, Quazi K.
    [J]. EARTH INTERACTIONS, 2009, 13 : 1 - 22
  • [6] Atmospheric Controls on Seasonal and Interannual Variations in the Precipitation Isotope in the East Asian Monsoon Region
    Cai, Zhongyin
    Tian, Lide
    [J]. JOURNAL OF CLIMATE, 2016, 29 (04) : 1339 - 1352
  • [7] Remote estimation of terrestrial evapotranspiration by Landsat 5 TM and the SEBAL model in cold and high-altitude regions: a case study of the upper reach of the Shule River Basin, China
    Chang, Yaping
    Ding, Yongjian
    Zhao, Qiudong
    Zhang, Shiqiang
    [J]. HYDROLOGICAL PROCESSES, 2017, 31 (03) : 514 - 524
  • [8] Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales
    Chen, Fahu
    Chen, Jianhui
    Huang, Wei
    Chen, Shengqian
    Huang, Xiaozhong
    Jin, Liya
    Jia, Jia
    Zhang, Xiaojian
    An, Chengbang
    Zhang, Jiawu
    Zhao, Yan
    Yu, Zicheng
    Zhang, Renhe
    Liu, Jianbao
    Zhou, Aifeng
    Feng, Song
    [J]. EARTH-SCIENCE REVIEWS, 2019, 192 : 337 - 354
  • [9] Spatiotemporal precipitation variations in the arid Central Asia in the context of global warming
    Chen FaHu
    Huang Wei
    Jin LiYa
    Chen JianHui
    Wang JinSong
    [J]. SCIENCE CHINA-EARTH SCIENCES, 2011, 54 (12) : 1812 - 1821
  • [10] [陈发虎 Chen Fahu], 2009, [地学前缘, Earth Science Frontiers], V16, P23