42 citations as recorded by crossref.

1. Moisture Source Changes Contributed to Different Precipitation Changes over the Northern and Southern Tibetan Plateau C. Zhang et al. 10.1175/JHM-D-18-0094.1
2. Latitudinal effects on phenology near the northern limit of figs in China H. Chen et al. 10.1038/s41598-018-22548-7
3. Ecological restoration enhances ecosystem health in the karst regions of southwest China C. Liao et al. 10.1016/j.ecolind.2018.03.036
4. Evaluation and application analysis of kilometer-scale convective parameters derived from a statistical downscaling method over Central China M. Shi et al. 10.1007/s00382-023-06820-9
5. Characteristics of Propagation of Meteorological to Hydrological Drought for Lake Baiyangdian in a Changing Environment S. He et al. 10.3390/atmos13091531
6. More frequent summer heat waves in southwestern China linked to the recent declining of Arctic sea ice K. Deng et al. 10.1088/1748-9326/ab8335
7. Uniformly elevated future heat stress in China driven by spatially heterogeneous water vapor changes F. Wang et al. 10.1038/s41467-024-48895-w
8. Moisture sources for precipitation in Southwest China in summer and the changes during the extreme droughts of 2006 and 2011 C. Zhang 10.1016/j.jhydrol.2020.125333
9. Examining moisture contribution for precipitation in response to climate change and anthropogenic factors in Hengduan Mountain Region, China X. Zhang et al. 10.1016/j.jhydrol.2023.129562
10. Wet-to-dry shift over Southwest China in 1994 tied to the warming of tropical warm pool L. Wang et al. 10.1007/s00382-018-4068-8
11. Improved understanding of how irrigated area expansion enhances precipitation recycling by land–atmosphere coupling X. Wang et al. 10.1016/j.agwat.2024.108904
12. Assessment and attribution of China’s droughts using an integrated drought index derived from GRACE and GRACE-FO data S. Deng et al. 10.1016/j.jhydrol.2021.127170
13. The Abrupt Change in Potential Evapotranspiration and Its Climatic Attribution over the Past 50 Years in the Sichuan–Chongqing Region, China Q. Zheng et al. 10.3390/atmos15070829
14. Global evaluation of the “dry gets drier, and wet gets wetter” paradigm from a terrestrial water storage change perspective J. Xiong et al. 10.5194/hess-26-6457-2022
15. Water storage redistribution over East China, between 2003 and 2015, driven by intra- and inter-annual climate variability Q. He et al. 10.1016/j.jhydrol.2019.124475
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17. Interdecadal Variability of Summer Precipitation Efficiency in East Asia J. Wang et al. 10.1155/2019/3563024
18. Difference in the atmospheric water cycle over the Hengduan Mountains between wet and dry summers Y. Zhao et al. 10.1002/joc.7533
19. Analysis of Drought Vulnerability Characteristics and Risk Assessment Based on Information Distribution and Diffusion in Southwest China S. Jiang et al. 10.3390/atmos9070239
20. Moisture sources of precipitation over the Pearl River Basin in South China X. Liu et al. 10.1002/joc.8447
21. Assessing the Roles of Terrestrial Stilling and Solar Dimming in Land Surface Drying/Wetting across China K. Duan et al. 10.3390/w12071996
22. Asymmetrical synchronization of extreme rainfall events in southwest China P. Qiao et al. 10.1002/joc.7569
23. Past, present, and future geo-biosphere interactions on the Tibetan Plateau and implications for permafrost T. Ehlers et al. 10.1016/j.earscirev.2022.104197
24. Evaluation of High-Resolution Precipitation Products over Southwest China Y. Nie & J. Sun 10.1175/JHM-D-20-0045.1
25. Why was Pakistan extreme precipitation stronger in 2022 than in 2010? X. Yuan et al. 10.1016/j.accre.2023.11.016
26. Complex Networks Reveal Teleconnections between the Global SST and Rainfall in Southwest China P. Qiao et al. 10.3390/atmos12010101
27. Can Satellite Precipitation Products Estimate Probable Maximum Precipitation: A Comparative Investigation with Gauge Data in the Dadu River Basin Y. Yang et al. 10.3390/rs10010041
28. Contributions of moisture sources to precipitation in the major drainage basins in the Tibetan Plateau Y. Li et al. 10.1007/s11430-021-9890-6
29. Spatiotemporal Differences in Dominants of Dryness/Wetness Changes in Southwest China S. Zhou et al. 10.1155/2019/2820769
30. Recent progress on the sources of continental precipitation as revealed by moisture transport analysis L. Gimeno et al. 10.1016/j.earscirev.2019.103070
31. Asian Winter Monsoon Imprint on the Water Column Structure at the Northern South China Sea Coast Y. Zhang et al. 10.3389/feart.2021.680180
32. Tracing anomalies in moisture recycling and transport to two record-breaking droughts over the Mid-to-Lower Reaches of the Yangtze River Y. Guan et al. 10.1016/j.jhydrol.2022.127787
33. An analysis on moisture source of extreme precipitation in Southwest China in summer C. ZHANG & S. WU 10.31497/zrzyxb.20210508
34. Asymmetric response of short- and long-duration dry spells to warming during the warm-rain season over Eastern monsoon China C. Li et al. 10.1016/j.jhydrol.2021.127114
35. Summer monsoon–induced upwelling dominated coastal sea surface temperature variations in the northern South China Sea over the last two millennia W. Lee et al. 10.1177/0959683618824715
36. Spatiotemporal Variations in Daytime and Night-Time Precipitation on the Yunnan–Guizhou Plateau from 1960 to 2017 D. Zhu et al. 10.3390/atmos13030415
37. Increase in summer precipitation over the Sichuan Basin in recent decades and possible causes Y. Nie & J. Sun 10.1002/joc.8086
38. Prolonged duration and increased severity of agricultural droughts during 1978 to 2016 detected by ESA CCI SM in the humid Yunnan Province, Southwest China S. Ma et al. 10.1016/j.catena.2020.105036
39. Drought Onset and Termination in India D. Shah & V. Mishra 10.1029/2020JD032871
40. Spatially differentiated changes in regional climate and underlying drivers in southwestern China M. Wang et al. 10.1007/s11676-021-01374-0
41. Synoptic‐Scale Circulation Precursors of Extreme Precipitation Events Over Southwest China During the Rainy Season Y. Nie & J. Sun 10.1029/2021JD035134
42. Changes in the moisture contribution over global arid regions C. Wang et al. 10.1007/s00382-022-06600-x