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Cross-Equatorial Flow as a Precursor of East-West Monsoon Precipitation Pattern in the Southern Tibetan Plateau

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inferredcites →https://doi.org/10.1002/2014jd022928openalex-extracted
The observed impacts of South Asian summer monsoon on the local atmosphere and the near‐surface turbulent heat exchange over the Southeast Tibet
inferredcites →https://doi.org/10.1002/2016gl072439openalex-extracted
Contribution of human influence to increased daily precipitation extremes over China
inferredcites →https://doi.org/10.1002/jgrd.50290openalex-extracted
Influences of the Atlantic Ocean on the summer precipitation of the southeastern Tibetan Plateau
inferredcites →https://doi.org/10.1002/qj.3803openalex-extracted
The ERA5 global reanalysis
inferredcites →https://doi.org/10.1002/rog.20023openalex-extracted
A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: Observations and simulations
inferredcites →https://doi.org/10.1007/s00382-017-3710-1openalex-extracted
Role of the meridional dipole of SSTA and associated cross-equatorial flow in the tropical eastern Pacific in terminating the 2014 El Niño development
inferredcites →https://doi.org/10.1007/s00382-018-4218-zopenalex-extracted
Potential regulation on the climatic effect of Tibetan Plateau heating by tropical air–sea coupling in regional models
inferredcites →https://doi.org/10.1007/s00704-013-0860-xopenalex-extracted
GPCC's new land surface precipitation climatology based on quality-controlled in situ data and its role in quantifying the global water cycle
inferredcites →https://doi.org/10.1007/s10584-014-1175-3openalex-extracted
Response of inland lake dynamics over the Tibetan Plateau to climate change
inferredcites →https://doi.org/10.1007/s10584-016-1877-9openalex-extracted
Spatiotemporal variations in volume of closed lakes on the Tibetan Plateau and their climatic responses from 1976 to 2013
inferredcites →https://doi.org/10.1007/s11430-022-1086-1openalex-extracted
The northern boundary of the Asian summer monsoon and division of westerlies and monsoon regimes over the Tibetan Plateau in present-day
inferredcites →https://doi.org/10.1016/j.accre.2023.11.016openalex-extracted
Why was Pakistan extreme precipitation stronger in 2022 than in 2010?
inferredcites →https://doi.org/10.1016/j.atmosres.2021.105875openalex-extracted
Characterizing the features of precipitation for the Tibetan Plateau among four gridded datasets: Detection accuracy and spatio-temporal variabilities
inferredcites →https://doi.org/10.1029/2008gl034330openalex-extracted
Tibetan Plateau warming and precipitation changes in East Asia
inferredcites →https://doi.org/10.1029/2011jd017012openalex-extracted
Water vapor transport for summer precipitation over the Tibetan Plateau: Multidata set analysis
inferredcites →https://doi.org/10.1029/2023gl104891openalex-extracted
Seasonally Evolving Trends Explain the North‐South Dipole Pattern Observed in Tibetan Plateau Precipitation
inferredcites →https://doi.org/10.1038/ncomms10925openalex-extracted
Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
inferredcites →https://doi.org/10.1038/s41467-023-44445-yopenalex-extracted
A stratospheric precursor of East Asian summer droughts and floods
inferredcites →https://doi.org/10.1038/s43017-022-00299-4openalex-extracted
The imbalance of the Asian water tower
inferredcites →https://doi.org/10.1073/pnas.1214626110openalex-extracted
Subtropical High predictability establishes a promising way for monsoon and tropical storm predictions
inferredcites →https://doi.org/10.1088/1748-9326/abcb36openalex-extracted
Mechanisms of the decadal variability of monsoon rainfall in the southern Tibetan Plateau
inferredcites →https://doi.org/10.1093/nsr/nwv061openalex-extracted
Mountain hazards in the Tibetan Plateau: research status and prospects
inferredcites →https://doi.org/10.1175/2008jcli2625.1openalex-extracted
Seasonality and Interannual Variability of the Westerly Jet in the Tibetan Plateau Region*
inferredcites →https://doi.org/10.1175/2010jcli2953.1openalex-extracted
Composite Structure of Monsoon Low Pressure Systems and Its Relation to Indian Rainfall
inferredcites →https://doi.org/10.1175/jcli-d-16-0914.1openalex-extracted
A Dipole Pattern of Summertime Rainfall across the Indian Subcontinent and the Tibetan Plateau
inferredcites →https://doi.org/10.1175/jcli-d-18-0319.1openalex-extracted
Intraseasonal Variability of Rainfall and Its Effect on Interannual Variability across the Indian Subcontinent and the Tibetan Plateau
inferredcites →https://doi.org/10.1175/jcli-d-22-0686.1openalex-extracted
Land–Atmosphere Interactions Partially Offset the Accelerated Tibetan Plateau Water Cycle through Dynamical Processes
inferredcites →https://doi.org/10.1175/jcli-d-22-0770.1openalex-extracted
Weakened Subtropical Westerlies Reduced Early Spring Precipitation in the Southeast Tibetan Plateau
inferredcites →https://doi.org/10.1360/n972015-00849openalex-extracted
Risk assessment and disaster reduction strategies for mountainous and meteorological hazards in Tibetan Plateau
inferredcites →https://doi.org/10.5194/tc-9-1229-2015openalex-extracted
Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994–2013)
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