95 citations as recorded by crossref.

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49. Spatial distribution and controlling factors of stable isotopes in meteoric waters on the Tibetan Plateau: Implications for paleoelevation reconstruction L. Li & C. Garzione 10.1016/j.epsl.2016.11.046
50. 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
51. Using stable isotopes of surface water and groundwater to quantify moisture sources across the Yellow River source region X. Kuang et al. 10.1002/hyp.13441
52. WRF‐based dynamical downscaling of ERA5 reanalysis data for High Mountain Asia: Towards a new version of the High Asia Refined analysis X. Wang et al. 10.1002/joc.6686
53. Manifestations and mechanisms of the Karakoram glacier Anomaly D. Farinotti et al. 10.1038/s41561-019-0513-5
54. A 14 ka high-resolution δ18O lake record reveals a paradigm shift for the process-based reconstruction of hydroclimate on the northern Tibetan Plateau B. Wünnemann et al. 10.1016/j.quascirev.2018.09.040
55. Climate variability rather than overstocking causes recent large scale cover changes of Tibetan pastures L. Lehnert et al. 10.1038/srep24367
56. Multi-centennial climate cycles and their impact on the Tubo Dynasty in the southern Tibetan Plateau H. Li et al. 10.1016/j.palaeo.2021.110584
57. Understanding precipitation recycling over the Tibetan Plateau using tracer analysis with WRF Y. Gao et al. 10.1007/s00382-020-05426-9
58. Can summer monsoon moisture invade the Jade Pass in Northwestern China? W. Du et al. 10.1007/s00382-020-05423-y
59. 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
60. High-elevation shrub-ring δ18O on the northern slope of the central Himalayas records summer (May–July) temperatures R. Huang et al. 10.1016/j.palaeo.2019.03.038
61. 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
62. Impact of model resolution on simulating the water vapor transport through the central Himalayas: implication for models’ wet bias over the Tibetan Plateau C. Lin et al. 10.1007/s00382-018-4074-x
63. Simulation of the dipole pattern of summer precipitation over the Tibetan Plateau by CMIP6 models W. Shang et al. 10.1088/1748-9326/abd0ac
64. Moisture and Temperature Covariability over the Southeastern Tibetan Plateau during the Past Nine Centuries J. Wang et al. 10.1175/JCLI-D-19-0363.1
65. A Generalized Evaluation Scheme for Comparing Temperature Products from Satellite Observations, Numerical Weather Model, and Ground Measurements Over the Tibetan Plateau X. Ouyang et al. 10.1109/TGRS.2018.2815272
66. The influence of tropical forcing on extreme winter precipitation in the western Himalaya F. Cannon et al. 10.1007/s00382-016-3137-0
67. Recent Changes in the Moisture Source of Precipitation over the Tibetan Plateau C. Zhang et al. 10.1175/JCLI-D-15-0842.1
68. 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
69. 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
70. Ecologic shift and aridification in the northern Tibetan Plateau revealed by leaf wax n-alkane δ2H and δ13C records M. Wu et al. 10.1016/j.palaeo.2018.11.005
71. Morphometric Controls on Glacier Mass Balance of the Puruogangri Ice Field, Central Tibetan Plateau L. Liu et al. 10.3390/w8110496
72. 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
73. 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
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76. Characterizing precipitation in high altitudes of the western Tibetan plateau with a focus on major glacier areas D. Li et al. 10.1002/joc.6509
77. Added Value of a Convection Permitting Model in Simulating Atmospheric Water Cycle Over the Asian Water Tower Y. Zhao et al. 10.1029/2021JD034788
78. Dust and sandstorm: ecosystem perspectives on dryland hazards in Northeast Asia: a review S. Kang et al. 10.1186/s41610-021-00205-x
79. Enhanced Recent Local Moisture Recycling on the Northwestern Tibetan Plateau Deduced From Ice Core Deuterium Excess Records W. An et al. 10.1002/2017JD027235
80. Remote moisture sources for 6-hour summer precipitation over the Southeastern Tibetan Plateau and its effects on precipitation intensity S. Yang et al. 10.1016/j.atmosres.2019.104803
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84. 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
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88. Lake water and glacier mass gains in the northwestern Tibetan Plateau observed from multi-sensor remote sensing data: Implication of an enhanced hydrological cycle G. Zhang et al. 10.1016/j.rse.2019.111554
89. Unexpected climate variability inferred from a 380-year tree-ring earlywood oxygen isotope record in the Karakoram, Northern Pakistan H. Zhu et al. 10.1007/s00382-021-05736-6
90. 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
91. Leaf unfolding of Tibetan alpine meadows captures the arrival of monsoon rainfall R. Li et al. 10.1038/srep20985
92. Increased El Niño–Southern Oscillation sensitivity of tree growth on the southern Tibetan Plateau since the 1970s X. Cheng et al. 10.1002/joc.6032
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