65 citations as recorded by crossref.

1. On the glacial-interglacial variability of the Asian monsoon in speleothem δ 18 O records G. Liu et al. 10.1126/sciadv.aay8189
2. Precipitation stable isotope records from the northern Hengduan Mountains in China capture signals of the winter India–Burma Trough and the Indian Summer Monsoon W. Yu et al. 10.1016/j.epsl.2017.08.018
3. Experimental determination and theoretical framework of kinetic fractionation at the water vapour–ice interface at low temperature M. Casado et al. 10.1016/j.gca.2015.11.009
4. Triple oxygen isotope variability of precipitation in a tropical mountainous region L. Arellano et al. 10.1016/j.gca.2024.09.024
5. Spatial distribution of 17O-excess in surface snow along a traverse from Zhongshan station to Dome A, East Antarctica H. Pang et al. 10.1016/j.epsl.2015.01.014
6. Ice core drilling on a high-elevation accumulation zone of Trambau Glacier in the Nepal Himalaya A. Tsushima et al. 10.1017/aog.2021.15
7. Satellite-Based Distribution of Inverse Altitude Effect of Global Water Vapor Isotopes: Potential Influences on Isotopes in Climate Proxies G. Yang et al. 10.3390/rs15184533
8. Lagrangian process attribution of isotopic variations in near-surface water vapour in a 30-year regional climate simulation over Europe M. Dütsch et al. 10.5194/acp-18-1653-2018
9. Deciphering key processes controlling rainfall isotopic variability during extreme tropical cyclones R. Sánchez-Murillo et al. 10.1038/s41467-019-12062-3
10. Oexcess17 in speleothem carbonates in Soreq Cave as an archive for hydro-climatic conditions H. Affek et al. 10.1016/j.epsl.2023.118366
11. Precipitation regime influence on oxygen triple-isotope distributions in Antarctic precipitation and ice cores M. Miller 10.1016/j.epsl.2017.10.035
12. Vehicle-based in situ observations of the water vapor isotopic composition across China: spatial and seasonal distributions and controls D. Wang et al. 10.5194/acp-23-3409-2023
13. Triple oxygen isotope compositions reveal transitions in the moisture source of West China Autumn Precipitation L. Sha et al. 10.1038/s43247-024-01354-2
14. Continental scale variation in 17O-excess of meteoric waters in the United States S. Li et al. 10.1016/j.gca.2015.04.047
15. The triple oxygen isotope composition of phytoliths as a proxy of continental atmospheric humidity: insights from climate chamber and climate transect calibrations A. Alexandre et al. 10.5194/bg-15-3223-2018
16. A framework for triple oxygen isotopes in speleothem paleoclimatology T. Huth et al. 10.1016/j.gca.2021.11.002
17. Surface processes and drivers of the snow water stable isotopic composition at Dome C, East Antarctica – a multi-dataset and modelling analysis I. Ollivier et al. 10.5194/tc-19-173-2025
18. Quantifying the Fingerprint of Oceanic Moisture Source Conditions in Deuterium and 17O Excess Parameters of Precipitation Z. Xia 10.1029/2022GL101901
19. Seasonal and ENSO Influences on the Stable Isotopic Composition of Galápagos Precipitation N. Martin et al. 10.1002/2017JD027380
20. Importance of the advection scheme for the simulation of water isotopes over Antarctica by atmospheric general circulation models: A case study for present-day and Last Glacial Maximum with LMDZ-iso A. Cauquoin et al. 10.1016/j.epsl.2019.115731
21. Dew-induced transpiration suppression impacts the water and isotope balances of Colocasia leaves C. Gerlein-Safdi et al. 10.1007/s00442-018-4199-y
22. Influence of Summer Sublimation on δD, δ18O, and δ17O in Precipitation, East Antarctica, and Implications for Climate Reconstruction From Ice Cores H. Pang et al. 10.1029/2018JD030218
23. The Seasonality of Deuterium Excess in Non‐Polar Precipitation Z. Xia et al. 10.1029/2021GB007245
24. Variability and Controls on δ18O, d‐excess, and ∆′17O in Southern Peruvian Precipitation P. Aron et al. 10.1029/2020JD034009
25. Isotope hydrology to provide insights into the behaviour of temporary wetlands as a basis for developing sustainable ecohydrological management strategies in Mediterranean regions A. Mattei et al. 10.1002/eco.2411
26. Global and local meteoric water lines for δ17O/δ18O and the spatiotemporal distribution of Δ′17O in Earth’s precipitation S. Terzer-Wassmuth et al. 10.1038/s41598-023-45920-8
27. Short-term variability in the dates of the Indian monsoon onset and retreat on the southern and northern slopes of the central Himalayas as determined by precipitation stable isotopes W. Yu et al. 10.1007/s00382-015-2829-1
28. Comparison of GCM-simulated isotopic compositions of precipitation in arid central Asia S. Wang et al. 10.1007/s11442-015-1201-z
29. Stable isotope modeling of the groundwater discharge in complex watersheds of the state of São Paulo, Brazil L. Santarosa et al. 10.1016/j.jsames.2022.104063
30. Paired stable isotopologues in precipitation and vapor: A case study of the amount effect within western tropical Pacific storms J. Conroy et al. 10.1002/2015JD023844
31. Intra-Event Trends in Stable Isotopes: Exploring Midlatitude Precipitation Using a Vertically Pointing Micro Rain Radar C. Muller et al. 10.1175/JHM-D-14-0038.1
32. Current state and future challenges in stable isotope applications of the tropical hydrologic cycle (Invited Commentary) M. Vuille 10.1002/hyp.11490
33. Geochemical evolution and seasonality of groundwater recharge at water-scarce southeast margin of the Chihuahuan Desert in Mexico P. Roy et al. 10.1016/j.envres.2021.111847
34. Deuterium excess as a proxy for continental moisture recycling and plant transpiration F. Aemisegger et al. 10.5194/acp-14-4029-2014
35. Triple Oxygen Isotope Systematics in the Hydrologic Cycle J. Surma et al. 10.2138/rmg.2021.86.12
36. A stable isotope toolbox for water and inorganic carbon cycle studies C. Hillaire-Marcel et al. 10.1038/s43017-021-00209-0
37. Stable isotope compositions (δ2H, δ18O and δ17O) of rainfall and snowfall in the central United States C. Tian et al. 10.1038/s41598-018-25102-7
38. Identification of sources and groundwater recharge zones from hydrochemistry and stable isotopes of an agriculture-based paleo-lacustrine basin of drought-prone northeast Mexico P. Roy et al. 10.1016/j.chemer.2021.125742
39. Exploring the potential of Δ17O in CO2 for determining mesophyll conductance G. Adnew et al. 10.1093/plphys/kiad173
40. Stable isotopic composition in snowpack along the traverse from a coastal location to Dome A (East Antarctica): Results from observations and numerical modeling T. Ma et al. 10.1016/j.polar.2020.100510
41. The Impact of Nonequilibrium and Equilibrium Fractionation on Two Different Deuterium Excess Definitions M. Dütsch et al. 10.1002/2017JD027085
42. The Forest Effects on the Isotopic Composition of Rainfall in the Northwestern Amazon Basin A. Ampuero et al. 10.1029/2019JD031445
43. Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters A. Touzeau et al. 10.5194/tc-10-837-2016
44. The Dominant Role of Brewer‐Dobson Circulation on 17O‐Excess Variations in Snow Pits at Dome A, Antarctica H. Pang et al. 10.1029/2022JD036559
45. Three-year monitoring of stable isotopes of precipitation at Concordia Station, East Antarctica B. Stenni et al. 10.5194/tc-10-2415-2016
46. Modelling water isotopologues (1H2H16O, 1H217O) in the coupled numerical climate model iLOVECLIM (version 1.1.5) T. Extier et al. 10.5194/gmd-17-2117-2024
47. Triple Oxygen Isotopes: Fundamental Relationships and Applications H. Bao et al. 10.1146/annurev-earth-060115-012340
48. The response and sensitivity of deuterium and 17O excess parameters in precipitation to hydroclimate processes Z. Xia et al. 10.1016/j.earscirev.2023.104432
49. Glacial–interglacial changes in H218O, HDO and deuterium excess – results from the fully coupled ECHAM5/MPI-OM Earth system model M. Werner et al. 10.5194/gmd-9-647-2016
50. Water isotopes – climate relationships for the mid-Holocene and preindustrial period simulated with an isotope-enabled version of MPI-ESM A. Cauquoin et al. 10.5194/cp-15-1913-2019
51. Seasonal and spatial variations of 17Oexcess and dexcess in Antarctic precipitation: Insights from an intermediate complexity isotope model S. Schoenemann & E. Steig 10.1002/2016JD025117
52. Continuous-Flow Analysis of δ17O, δ18O, and δD of H2O on an Ice Core from the South Pole E. Steig et al. 10.3389/feart.2021.640292
53. Review on Applications of 17O in Hydrological Cycle Y. Nyamgerel et al. 10.3390/molecules26154468
54. Regional atmospheric dynamics govern interannual and seasonal stable isotope composition in southeastern Brazil V. dos Santos et al. 10.1016/j.jhydrol.2019.124136
55. What controls deuterium excess in global precipitation? S. Pfahl & H. Sodemann 10.5194/cp-10-771-2014
56. A Climatology of Strong Large-Scale Ocean Evaporation Events. Part II: Relevance for the Deuterium Excess Signature of the Evaporation Flux F. Aemisegger & J. Sjolte 10.1175/JCLI-D-17-0592.1
57. Understanding Tropical Convection Through Triple Oxygen Isotopes of Precipitation From the Maritime Continent S. He et al. 10.1029/2020JD033418
58. Triple oxygen isotopes in the water cycle P. Aron et al. 10.1016/j.chemgeo.2020.120026
59. Triple isotopes (δD, δ18O, δ17O) characteristic of river water and groundwater in an arid watershed from Qaidam Basin, Northwestern China: implications for hydrological cycle N. Yang et al. 10.1016/j.scitotenv.2024.172229
60. Tropical precipitation anomalies and d -excess evolution during El Niño 2014-16 R. Sánchez-Murillo et al. 10.1002/hyp.11088
61. Triple oxygen isotope fractionation between CaCO3 and H2O in inorganically precipitated calcite and aragonite N. Voarintsoa et al. 10.1016/j.chemgeo.2020.119500
62. Triple oxygen isotope compositions of globally distributed soil carbonates record widespread evaporation of soil waters J. Kelson et al. 10.1016/j.gca.2023.06.034
63. Carbonate 17Oexcess as a paleo-hydrology proxy: Triple oxygen isotope fractionation between H2O and biogenic aragonite, derived from freshwater mollusks S. Bergel et al. 10.1016/j.gca.2020.02.005
64. Large-scale atmospheric circulation influences the ice core d-excess record from the central Tibetan Plateau L. Shao et al. 10.1007/s00382-021-05779-9
65. Interannual variation of water isotopologues at Vostok indicates a contribution from stratospheric water vapor R. Winkler et al. 10.1073/pnas.1215209110