140 citations as recorded by crossref.

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8. Effects of horizontal resolution and air–sea coupling on simulated moisture source for East Asian precipitation in MetUM GA6/GC2 L. Guo et al. 10.5194/gmd-13-6011-2020
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16. Intensified Atmospheric Branch of the Hydrological Cycle Over the Tibetan Plateau During the Last Interglacial From a Dynamical Downscaling Perspective N. Jiang et al. 10.1029/2022JD036470
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19. What induces the interdecadal shift of the dipole patterns of summer precipitation trends over the Tibetan Plateau? Y. Liu et al. 10.1002/joc.7122
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23. Comprehensive estimation of lake volume changes on the Tibetan Plateau during 1976–2019 and basin-wide glacier contribution G. Zhang et al. 10.1016/j.scitotenv.2021.145463
24. Spatial patterns and possible mechanisms of precipitation changes in recent decades over and around the Tibetan Plateau in the context of intense warming and weakening winds X. Guo & L. Tian 10.1007/s00382-022-06197-1
25. Scale effects of topographic ruggedness on precipitation over Qinghai‐Tibet Plateau N. Lu 10.1002/asl.904
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30. Improving daily precipitation estimates for the Qinghai‐Tibetan plateau based on environmental similarity Y. Wang et al. 10.1002/joc.6523
31. Atmospheric moisture transport versus precipitation across the Tibetan Plateau: A mini-review and current challenges Y. Ma et al. 10.1016/j.atmosres.2018.03.015
32. 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
33. South Asian black carbon is threatening the water sustainability of the Asian Water Tower J. Yang et al. 10.1038/s41467-022-35128-1
34. Controls of the recent precipitation anomalies in the southeastern Tibetan Plateau: from the perspective of Indian summer monsoon activities and moisture sources X. Guo et al. 10.1007/s00382-023-06919-z
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36. Temporal variations of stable isotopic compositions in atmospheric water vapor on the Southeastern Tibetan Plateau and their controlling factors M. Chen et al. 10.1016/j.atmosres.2024.107328
37. Can summer monsoon moisture invade the Jade Pass in Northwestern China? W. Du et al. 10.1007/s00382-020-05423-y
38. A Bigger Picture of how the Tibetan Lakes Have Changed Over the Past Decade Revealed by CryoSat‐2 Altimetry L. Jiang et al. 10.1029/2020JD033161
39. Self-organizing map network-based precipitation regionalization for the Tibetan Plateau and regional precipitation variability N. Wang & J. Yin 10.1007/s00704-017-2349-5
40. Climatology of near-surface wind speed from observational, reanalysis and high-resolution regional climate model data over the Tibetan Plateau L. Minola et al. 10.1007/s00382-023-06931-3
41. Quantifying the Spatio-Temporal Pattern Differences in Climate Change before and after the Turning Year in Southwest China over the Past 120 Years M. Wang et al. 10.3390/atmos14060940
42. Recent Changes in the Moisture Source of Precipitation over the Tibetan Plateau C. Zhang et al. 10.1175/JCLI-D-15-0842.1
43. Spatially coherent clusters of summer precipitation extremes in the Tibetan Plateau: Where is the moisture from? Y. Ma et al. 10.1016/j.atmosres.2020.104841
44. Use of δ 18 O atm in dating a Tibetan ice core record of Holocene/Late Glacial climate L. Thompson et al. 10.1073/pnas.2205545119
45. Chemical and isotopic (O, H, C) composition of surface waters in the catchment of Lake Donggi Cona (NW China) and implications for paleoenvironmental reconstructions M. Weynell et al. 10.1016/j.chemgeo.2016.04.012
46. Morphometric Controls on Glacier Mass Balance of the Puruogangri Ice Field, Central Tibetan Plateau L. Liu et al. 10.3390/w8110496
47. Identifying and contrasting the sources of the water vapor reaching the subregions of the Tibetan Plateau during the wet season B. Chen et al. 10.1007/s00382-019-04963-2
48. Air mass origin signals in δ 18O of tree-ring cellulose revealed by back-trajectory modeling at the monsoonal Tibetan plateau J. Wernicke et al. 10.1007/s00484-016-1292-y
49. Survival of the Qaidam mega-lake system under mid-Pliocene climates and its restoration under future climates D. Scherer 10.5194/hess-24-3835-2020
50. Connections Between a Late Summer Snowstorm Over the Southwestern Tibetan Plateau and a Concurrent Indian Monsoon Low‐Pressure System W. Dong et al. 10.1029/2018JD029710
51. Added Value of a Convection Permitting Model in Simulating Atmospheric Water Cycle Over the Asian Water Tower Y. Zhao et al. 10.1029/2021JD034788
52. Cenozoic paleoelevation history of the Lunpola Basin in Central Tibet: New evidence from volcanic glass hydrogen isotopes and a critical review L. Li et al. 10.1016/j.earscirev.2022.104068
53. Enhanced Recent Local Moisture Recycling on the Northwestern Tibetan Plateau Deduced From Ice Core Deuterium Excess Records W. An et al. 10.1002/2017JD027235
54. The enhanced relationship between summer rainfall over the eastern Tibetan Plateau and sea surface temperature in the tropical Indo-Pacific Ocean Q. Ren et al. 10.1007/s00382-022-06509-5
55. Spatio-Temporal Variations of Water Vapor Budget over the Tibetan Plateau in Summer and Its Relationship with the Indo-Pacific Warm Pool D. Meng et al. 10.3390/atmos11080828
56. The evolution of hydroclimate in Asia over the Cenozoic: A stable-isotope perspective J. Caves Rugenstein & C. Chamberlain 10.1016/j.earscirev.2018.09.003
57. The contributions of local and remote atmospheric moisture fluxes to East Asian precipitation and its variability L. Guo et al. 10.1007/s00382-017-4064-4
58. Global Climate Impacts of Land‐Surface and Atmospheric Processes Over the Tibetan Plateau J. Huang et al. 10.1029/2022RG000771
59. Projected changes in precipitation recycling over the Tibetan Plateau based on a global and regional climate model H. Zhang & Y. Gao 10.1175/JHM-D-21-0011.1
60. Spatiotemporal distribution of river water stable isotope compositions and variability of lapse rate in the central Rocky Mountains: Controlling factors and implications for paleoelevation reconstruction L. Zhu et al. 10.1016/j.epsl.2018.05.047
61. Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products Z. Zhang et al. 10.3390/rs10071031
62. Glacier melt buffers river runoff in the Pamir Mountains E. Pohl et al. 10.1002/2016WR019431
63. Climatology of Tibetan Plateau Vortices in Reanalysis Data and a High-Resolution Global Climate Model J. Curio et al. 10.1175/JCLI-D-18-0021.1
64. Air moisture signals in a stable oxygen isotope chronology of dwarf shrubs from the central Tibetan Plateau J. Wernicke et al. 10.1093/aob/mcz030
65. Long-term drying trend during 51.8–37.5 Ma in the Nangqian Basin, central-eastern Qinghai–Tibet Plateau S. Li et al. 10.3389/feart.2022.866304
66. Existence of Glacier Anomaly in the Interior and Northern Tibetan Plateau between 2000 and 2012 L. Liu et al. 10.3390/rs14132962
67. Summertime atmospheric water vapor transport between Tibetan Plateau and its surrounding regions during 1990–2019: Boundary discrepancy and interannual variation L. Sun et al. 10.1016/j.atmosres.2022.106237
68. Winter westerly disturbance dynamics and precipitation in the western Himalaya and Karakoram: a wave-tracking approach F. Cannon et al. 10.1007/s00704-015-1489-8
69. Interannual Variability of Precipitation Recycle Ratio Over the Tibetan Plateau Y. Zhao & T. Zhou 10.1029/2020JD033733
70. Added value of kilometer-scale modeling over the third pole region: a CORDEX-CPTP pilot study X. Zhou et al. 10.1007/s00382-021-05653-8
71. Precipitation efficiency of cloud and its influencing factors over the Tibetan plateau P. Zhao et al. 10.1002/joc.7251
72. Atmospheric moisture budget and its regulation on the variability of summer precipitation over the Tibetan Plateau Z. Wang et al. 10.1002/2016JD025515
73. Characteristics of Historical Precipitation in High Mountain Asia Based on a 15-Year High Resolution Dynamical Downscaling C. Riley et al. 10.3390/atmos12030355
74. High-altitude tree growth responses to climate change across the Hindu Kush Himalaya L. Zheng et al. 10.1093/jpe/rtab035
75. Local Climatic Factors Mediated Impacts of Large-Scale Climate Oscillations on the Growth of Vegetation Across the Tibetan Plateau L. Zhang et al. 10.3389/fenvs.2021.597971
76. Teleconnection between Summer NAO and East China Rainfall Variations: A Bridge Effect of the Tibetan Plateau Z. Wang et al. 10.1175/JCLI-D-17-0413.1
77. Quantification of Evaporative Sources of Precipitation and Its Changes in the Southeastern Tibetan Plateau and Middle Yangtze River Basin Y. Xu & Y. Gao 10.3390/atmos10080428
78. Central Asia's spatiotemporal glacier response ambiguity due to data inconsistencies and regional simplifications M. Barandun & E. Pohl 10.5194/tc-17-1343-2023
79. Precipitation Retrieval over the Tibetan Plateau from the Geostationary Orbit—Part 1: Precipitation Area Delineation with Elektro-L2 and Insat-3D C. Kolbe et al. 10.3390/rs11192302
80. Late Quaternary lacustrine Ostracoda and their implications for hydro-climatic variation in Northeastern Tibetan Plateau D. Yan et al. 10.1016/j.earscirev.2020.103251
81. Possible widths of Indian summer monsoon trajectories in Tibetan Plateau revealed by the direction of maximum summer precipitation decreases in recent decades X. Guo et al. 10.1007/s00382-022-06446-3
82. Characterizing potential sources and transport pathways of intense moisture during extreme precipitation events over the Tibetan Plateau O. Ayantobo et al. 10.1016/j.jhydrol.2022.128734
83. Evaluation of the near-surface climate of the recent global atmospheric reanalysis for Qilian Mountains, Qinghai-Tibet Plateau B. Huai et al. 10.1016/j.atmosres.2020.105401
84. C4 expansion of Central Asia in the middle Miocene linked to the strengthening Indian monsoon J. Wang et al. 10.1016/j.gloplacha.2023.104096
85. MODIS-derived interannual variability of the equilibrium-line altitude across the Tibetan Plateau M. Spiess et al. 10.3189/2016AoG71A014
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88. Multi-decadal periods of enhanced aeolian activity on the north-eastern Tibet Plateau during the last 2ka G. Stauch 10.1016/j.quascirev.2016.07.027
89. The elevation gradient of stable isotopes in precipitation in the eastern margin of Tibetan Plateau J. Li & Z. Pang 10.1007/s11430-021-9942-0
90. Weakening summer westerly circulation actuates greening of the Tibetan Plateau Z. Wang et al. 10.1016/j.gloplacha.2022.104027
91. Can Water Vapor Transport over the Himalayas above 8000 m asl?—A Case Study on Mt. Everest B. Xu et al. 10.3390/w14111671
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