All Stories

  1. The Quantitative Role of Moisture and Vertical Motion in Shaping Summer Heavy Rainfall over North China under Two Distinct Large-Scale Weather Patterns
  2. A Deep‐Learning Ensemble Method to Detect Atmospheric Rivers and Its Application to Projected Changes in Precipitation Regime
  3. The Critical Role of the Upper-Level Synoptic Disturbance on the China Henan “21.7” Extreme Precipitation Event
  4. Influence of stratosphere-to-troposphere transport on summertime surface O3 changes in North China Plain in 2019
  5. Importance of Diabatic Heating for the Eastward-Moving Heavy Rainfall Events along the Yangtze River, China
  6. Cloud Response Is Significantly Biased by CMIP6 Over the Tibetan Plateau
  7. The Remote Effect of Binary Typhoon Infa and Cempaka on the “21.7” Heavy Rainfall in Henan Province, China
  8. Anomalous surface O3 changes in North China Plain during the northwestward movement of a landing typhoon
  9. Correction to: Future precipitation changes in three key sub-regions of East Asia: the roles of thermodynamics and dynamics
  10. Improving the Estimate of Summer Daytime Planetary Boundary Layer Height Over Land From GPS Radio Occultation Data
  11. A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change
  12. Quantitative Attribution of Vertical Motion Responsible for Summer Heavy Rainfall Over North China
  13. Future precipitation changes in three key sub-regions of East Asia: the roles of thermodynamics and dynamics
  14. Intensity and microphysical properties surrounding the rapid intensification in landfalling Super Typhoons over China during the summer and autumn seasons
  15. How Were the Eastward-Moving Heavy Rainfall Events from the Tibetan Plateau to the Lower Reaches of the Yangtze River Enhanced?
  16. The Impact of the Observation Data Assimilation on Atmospheric Reanalyses over Tibetan Plateau and Western Yunnan-Guizhou Plateau
  17. Projection of Future Summer Precipitation over the Yellow River Basin: A Moisture Budget Perspective
  18. Why are there more summer afternoon low clouds over the Tibetan Plateau compared to eastern China?
  19. Statistical Characteristics and Synoptic Situations of Long‐Duration Heavy Rainfall Events Over North China
  20. Impact of Model Bias Correction on a Hybrid Data Assimilation System
  21. Spatiotemporal variation in the impact of meteorological conditions on PM2.5 pollution in China from 2000 to 2017
  22. Climate modulation of summer rainstorm activity in eastern China based on the Tibetan Plateau spring heating
  23. Enhancement of the summer extreme precipitation over North China by interactions between moisture convergence and topographic settings
  24. Association of Climate-related Total Atmospheric Energy Anomalies in the Tibetan Plateau with Haze in Eastern China
  25. Influence of Thermal Effects on Qinghai-Tibet Plateau on Air Quality in Typical Regions of China in Winter
  26. The Large‐Scale Circulation Patterns Responsible for Extreme Precipitation Over the North China Plain in Midsummer
  27. Effect of the Asian Water Tower over the Qinghai-Tibet Plateau and the characteristics of atmospheric water circulation
  28. Effects of convection over the Tibetan Plateau on rainstorms downstream of the Yangtze River Basin
  29. Vertical Structures of Dust Aerosols over East Asia Based on CALIPSO Retrievals
  30. Diurnal Variations in Summer Precipitation over the Yellow River Basin
  31. Effects of the Tibetan Plateau and its second staircase terrain on rainstorms over North China: From the perspective of water vapour transport
  32. Impact of Meteorological Conditions on PM2.5 Pollution in China during Winter
  33. The severity of drought and precipitation prediction in the eastern fringe of the Tibetan Plateau
  34. Trends in observed mean and extreme precipitation within the Yellow River Basin, China
  35. The Third Atmospheric Scientific Experiment for Understanding the Earth–Atmosphere Coupled System over the Tibetan Plateau and Its Effects
  36. Precursory strong-signal characteristics of the convective clouds of the Central Tibetan Plateau detected by radar echoes with respect to the evolutionary processes of an eastward-moving heavy rainstorm belt in the Yangtze River Basin
  37. Are precipitation anomalies associated with aerosol variations over eastern China?
  38. The upstream “strong signals” of the water vapor transport over the Tibetan Plateau during a heavy rainfall event in the Yangtze River Basin
  39. Extreme precipitation events in East China and associated moisture transport pathways