13 citations as recorded by crossref.

1. Coupling the Glacio-hydrological Degree-day Model (GDM) with PCRaster for spatial dynamic modeling of Himalayan river basins K. Shrestha et al. 10.5194/piahs-387-25-2024
2. Water sources and threshold behaviors of streamflow generation in a mountain headwater catchment X. Chen et al. 10.1016/j.jhydrol.2024.132117
3. Longer simulation time step of the tracer-aided hydrological model estimates lower contribution of slow runoff components Y. Nan et al. 10.1016/j.jhydrol.2023.129889
4. How and when glacial runoff is important: Tracing dynamics of meltwater and rainfall contribution to river runoff from headwaters to lowland in the Caucasus Mountains E. Rets et al. 10.1016/j.scitotenv.2024.172201
5. Runoff component quantification and future streamflow projection in a large mountainous basin based on a multidata-constrained cryospheric–hydrological model M. Zhang et al. 10.5194/hess-29-1033-2025
6. Groundwater dominance in streamflow generation: Insights from stable isotopes and tritium tracing in a semi-humid monsoonal catchment Z. Xu et al. 10.1016/j.ejrh.2025.102847
7. Separating snow and ice melt using water stable isotopes and glacio-hydrological modelling: towards improving the application of isotope analyses in highly glacierized catchments T. Müller et al. 10.5194/tc-19-423-2025
8. Simultaneous Separation of Runoff Pathways and Storage Times via Coupled Electrical Conductivity Mass Balance and Nonlinear Storage‐Discharge Relationship: Theory and Application Testing W. Yang et al. 10.1029/2024WR039052
9. Glaciers determine the sensitivity of hydrological processes to perturbed climate in a large mountainous basin on the Tibetan Plateau Y. Nan & F. Tian 10.5194/hess-28-669-2024
10. Isotope data-constrained hydrological model improves soil moisture simulation and runoff source apportionment Y. Nan & F. Tian 10.1016/j.jhydrol.2024.131006
11. Large scale hydrologic and tracer aided modelling: A review T. Stadnyk & T. Holmes 10.1016/j.jhydrol.2023.129177
12. Regional contributions of climate change and human activities to altered flow of the Lancang-mekong river K. Zhang et al. 10.1016/j.ejrh.2023.101535
13. Glacier meltwater has limited contributions to the total runoff in the major rivers draining the Tibetan Plateau Y. Nan et al. 10.1038/s41612-025-01060-6