134 citations as recorded by crossref.

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23. The residence time of water in the atmosphere revisited R. van der Ent & O. Tuinenburg 10.5194/hess-21-779-2017
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31. Towards an understanding of uncertainties in the Lagrangian analysis of moisture sources for tropical cyclone precipitation through a study case A. Pérez-Alarcón et al. 10.1016/j.atmosres.2024.107822
32. Analysis of Kenya’s Atmospheric Moisture Sources and Sinks P. Keys et al. 10.1175/EI-D-21-0016.1
33. The Zonal Patterns in Late Quaternary Tropical South American Precipitation T. Kukla et al. 10.1029/2022PA004498
34. Comparing deuterium excess to large-scale precipitation recycling models in the tropics S. Cropper et al. 10.1038/s41612-021-00217-3
35. Causes for overestimation of the moisture recycling in an alpine meadow ecosystem of the Shule River Basin, Tibetan Plateau, China H. Liu et al. 10.1016/j.jhydrol.2024.132226
36. The Atmospheric Moisture Residence Time and Reference Time for Moisture Tracking over China N. Wang et al. 10.1175/JHM-D-17-0204.1
37. Variability of Precipitation Recycling and Moisture Sources over the Colombian Pacific Region: A Precipitationshed Approach A. Enciso et al. 10.3390/atmos13081202
38. Atmospheric recycling of agricultural evapotranspiration in the Tarim Basin K. Shi et al. 10.3389/feart.2022.950299
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40. An analysis on moisture source of extreme precipitation in Southwest China in summer C. ZHANG & S. WU 10.31497/zrzyxb.20210508
41. Revealing Invisible Water: Moisture Recycling as an Ecosystem Service P. Keys et al. 10.1371/journal.pone.0151993
42. Landscape matters: Insights from the impact of mega-droughts on Colombia's energy transition W. Weng et al. 10.1016/j.eist.2020.04.003
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44. The Contribution of Transpiration to Precipitation Over African Watersheds S. Te Wierik et al. 10.1029/2021WR031721
45. Contribution of recycled moisture to local precipitation in the inland Heihe River Basin L. Zhao et al. 10.1016/j.agrformet.2019.03.014
46. Importance in Shifting Circulation Patterns for Dry Season Moisture Sources in the Brazilian Amazon Y. Mu et al. 10.1029/2023GL103167
47. Increasing Selin Co Lake Area in the Tibet Plateau with Its Moisture Cycle G. Wang et al. 10.3390/su17052024
48. Comparison of recycled vapor contribution to precipitation in urban vs. rural area—A case study in western China P. Zhao et al. 10.3389/fevo.2022.1012071
49. Aerial river management by smart cross-border reforestation W. Weng et al. 10.1016/j.landusepol.2019.03.010
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52. Upwind moisture supply increases risk to water security J. Posada-Marín et al. 10.1038/s44221-024-00291-w
53. Amazonian Moisture Recycling Revisited Using WRF With Water Vapor Tracers F. Dominguez et al. 10.1029/2021JD035259
54. Reviewing the Impact of Land Use and Land‐Use Change on Moisture Recycling and Precipitation Patterns S. te Wierik et al. 10.1029/2020WR029234
55. An Earth system law perspective on governing social-hydrological systems in the Anthropocene H. Ahlström et al. 10.1016/j.esg.2021.100120
56. Anomalous moisture sources of the Rhine basin during the extremely dry summers of 2003 and 2018 I. Benedict et al. 10.1016/j.wace.2020.100302
57. Arboreal Epiphytes in the Soil-Atmosphere Interface: How Often Are the Biggest “Buckets” in the Canopy Empty? H. Hargis et al. 10.3390/geosciences9080342
58. The Seasonality of Deuterium Excess in Non‐Polar Precipitation Z. Xia et al. 10.1029/2021GB007245
59. Effects of Continental Evaporation for Precipitation Over East Asia in the Past and the Future of HadGEM2-AO Climate Model J. Kim et al. 10.14191/Atmos.2016.26.4.553
60. Tracking the global flows of atmospheric moisture and associated uncertainties O. Tuinenburg & A. Staal 10.5194/hess-24-2419-2020
61. An abrupt shift in gross primary productivity over Eastern China-Mongolia and its inter-model diversity in land surface models D. Lee et al. 10.1038/s41598-023-49763-1
62. Advancing understanding of land–atmosphere interactions by breaking discipline and scale barriers J. Vilà‐Guerau de Arellano et al. 10.1111/nyas.14956
63. The Climatic Energy Balance Diagram (CEBD) highlights changes in the hydrological cycle of the Danube River basin L. Báder 10.2478/johh-2025-0001
64. A unified framework to estimate the origins of atmospheric moisture and heat using Lagrangian models J. Keune et al. 10.5194/gmd-15-1875-2022
65. Role of reservoir regulation and groundwater feedback in a simulated ground‐soil‐vegetation continuum: A long‐term regional scale analysis J. Wei et al. 10.1002/hyp.14341
66. A coupled equilibrium boundary layer model with stable water isotopes and its application to local water recycling K. Xiao et al. 10.1016/j.agrformet.2023.109572
67. Changes in Climate and Land Use Over the Amazon Region: Current and Future Variability and Trends J. Marengo et al. 10.3389/feart.2018.00228
68. The growing importance of oceanic moisture sources for continental precipitation L. Gimeno et al. 10.1038/s41612-020-00133-y
69. Effects of phenology and meteorological disturbance on litter rainfall interception for a Pinus elliottii stand in the Southeastern United States J. Van Stan et al. 10.1002/hyp.11292
70. 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
71. Rising Temperatures Increase Importance of Oceanic Evaporation as a Source for Continental Precipitation K. Findell et al. 10.1175/JCLI-D-19-0145.1
72. A Joint Impact on Water Vapor Transport over South China during the Pre-Rainy Season by ENSO and PDO G. Zhang et al. 10.3390/w14223639
73. Phenophase-based comparison of field observations to satellite-based actual evaporation estimates of a natural woodland: miombo woodland, southern Africa H. Zimba et al. 10.5194/hess-27-1695-2023
74. Atmospheric water recycling an essential feature of critical natural asset stewardship P. Keys et al. 10.1017/sus.2023.24
75. On the importance of plant phenology in the evaporative process of a semi-arid woodland: could it be why satellite-based evaporation estimates in the miombo differ? H. Zimba et al. 10.5194/hess-28-3633-2024
76. The influence of the precipitation recycling process on the shift to heavy precipitation over the Tibetan Plateau in the summer B. Zhang et al. 10.3389/feart.2023.1078501
77. The competing effects of terrestrial evapotranspiration and raindrop re-evaporation on the deuterium excess of continental precipitation Z. Xia & M. Winnick 10.1016/j.epsl.2021.117120
78. Self-amplified Amazon forest loss due to vegetation-atmosphere feedbacks D. Zemp et al. 10.1038/ncomms14681
79. Changes in a river's regime of a watercourse after a small water reservoir construction R. Fiala et al. 10.17221/23/2019-SWR
80. Can Landsat-Derived Variables Related to Energy Balance Improve Understanding of Burn Severity From Current Operational Techniques? A. Fernández-Manso et al. 10.3390/rs12050890
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82. Root zone in the Earth system H. Gao et al. 10.5194/hess-28-4477-2024
83. Contribution of recycled moisture to precipitation in oases of arid central Asia: A stable isotope approach S. Wang et al. 10.1002/2015WR018135
84. Observed Soil Moisture–Precipitation Feedback in Illinois: A Systematic Analysis over Different Scales H. Duerinck et al. 10.1175/JHM-D-15-0032.1
85. The Role of Plant CO2 Physiological Forcing in Shaping Future Daily-Scale Precipitation C. Skinner et al. 10.1175/JCLI-D-16-0603.1
86. Recent global decline in rainfall interception loss due to altered rainfall regimes X. Lian et al. 10.1038/s41467-022-35414-y
87. The Contribution of Local and Remote Transpiration, Ground Evaporation, and Canopy Evaporation to Precipitation Across North America T. Harrington et al. 10.1029/2022JD037290
88. Ocean and land moisture contributions to Midwest United States summertime precipitation C. Sala 10.1007/s00382-025-07617-8
89. Hydroclimatic Effects of a Hydropower Reservoir in a Tropical Hydrological Basin D. Zamora et al. 10.3390/su12176795
90. A water-function-based framework for understanding and governing water resilience in the Anthropocene M. Falkenmark & L. Wang-Erlandsson 10.1016/j.oneear.2021.01.009
91. Why was Pakistan extreme precipitation stronger in 2022 than in 2010? X. Yuan et al. 10.1016/j.accre.2023.11.016
92. Forests, atmospheric water and an uncertain future: the new biology of the global water cycle D. Sheil 10.1186/s40663-018-0138-y
93. Global terrestrial moisture recycling in Shared Socioeconomic Pathways A. Staal et al. 10.5194/esd-16-215-2025
94. Connection of Quasi-Resonant Amplification to the Delay in Atmospheric Residence Times Over India T. Lakshmi Kumar et al. 10.3389/feart.2021.615325
95. High-resolution global atmospheric moisture connections from evaporation to precipitation O. Tuinenburg et al. 10.5194/essd-12-3177-2020
96. Feedback between drought and deforestation in the Amazon A. Staal et al. 10.1088/1748-9326/ab738e
97. Reforestation effects on low flows: Review of public perceptions and scientific evidence I. van Meerveld & J. Seibert 10.1002/wat2.1760
98. Unraveling the discrepancies between Eulerian and Lagrangian moisture tracking models in monsoon- and westerly-dominated basins of the Tibetan Plateau Y. Li et al. 10.5194/acp-24-10741-2024
99. Recent progress on the sources of continental precipitation as revealed by moisture transport analysis L. Gimeno et al. 10.1016/j.earscirev.2019.103070
100. Recent decrease in summer precipitation over the Iberian Peninsula closely links to reduction in local moisture recycling Y. Liu et al. 10.5194/hess-26-1925-2022
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108. The importance of considering rainfall partitioning in afforestation initiatives in semiarid climates: A comparison of common planted tree species in Tehran, Iran S. Sadeghi et al. 10.1016/j.scitotenv.2016.06.048
109. Decline in Terrestrial Moisture Sources of the Mississippi River Basin in a Future Climate I. Benedict et al. 10.1175/JHM-D-19-0094.1
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129. Precession‐ and Obliquity‐Induced Changes in Moisture Sources for Enhanced Precipitation Over the Mediterranean Sea J. Bosmans et al. 10.1029/2019PA003655
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131. 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
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