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Arid Land Geography ›› 2026, Vol. 49 ›› Issue (2): 332-342.doi: 10.12118/j.issn.1000-6060.2025.180

• Climatology and Hydrology • Previous Articles     Next Articles

Impact of westerly-monsoon synergistic interaction on summer precipitation over the Tibetan Plateau

ZHANG Lu1,2(), ZHOU Bingrong3, YAN Yuqian1,3(), CAO Xiaoyun1,3, MA Youxuan2   

  1. 1. Key Laboratory of Disaster Prevention and Mitigation of Qinghai Province, Xining 810001, Qinghai, China
    2. Climate Center of Qinghai Province, Xining 810001, Qinghai, China
    3. Institute of Qinghai Meteorological Science Research, Xining 810001, Qinghai, China
  • Received:2025-04-10 Revised:2025-07-07 Online:2026-02-25 Published:2026-02-27
  • Contact: YAN Yuqian E-mail:zhanglu_0905@126.com;yan_yq1113@sina.com

Abstract:

Using the CN05.1 precipitation dataset and the NCEP/NCAR reanalysis data, this study examines the spatiotemporal characteristics of summer precipitation on the Tibetan Plateau from 1981 to 2022 and explores the influence of westerly-monsoon synergy on this precipitation. The results show that: (1) Average summer precipitation over the past four decades is 216.6 mm, with a spatial pattern that decreases from the southeast to the northwest and an increasing trend of 4.85 mm per decade. The first empirical orthogonal function (EOF) mode indicates a spatially coherent change across the plateau, with a notable increase in wetness observed in the late 2010s, while the second EOF mode reveals pronounced interdecadal variability. (2) The westerly-monsoon synergy index provides a more robust indicator of summer precipitation over the plateau than individual westerly and monsoon indices, with a correlation coefficient of 0.5, effectively capturing interannual variability. (3) The westerly-monsoon synergy exerts a significant influence on summer precipitation over the Tibetan Plateau. When the synergistic effect strengthens, the upper-level divergent westerly circulation interacts with low-level warm and moist air transported by the westerlies, enhancing vertical ascent and promoting precipitation. Conversely, when the synergy is weak, anomalous easterly circulation dominates, accompanied by low-level dry and cold northerly flows, under which subsidence and moisture divergence suppress precipitation formation.

Key words: summer precipitation, summer monsoon, westerlies, water vapor transport, synergistic interaction, Tibetan Plateau