15 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.
2. Water sources and threshold behaviors of streamflow generation in a mountain headwater catchment X. Chen et al.
3. Longer simulation time step of the tracer-aided hydrological model estimates lower contribution of slow runoff components Y. Nan et al.
4. Reducing hydrological uncertainty in large mountainous basins: the role of isotope, snow cover, and glacier dynamics in capturing streamflow seasonality D. Avesani et al.
5. 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.
6. Runoff component quantification and future streamflow projection in a large mountainous basin based on a multidata-constrained cryospheric–hydrological model M. Zhang et al.
7. Groundwater dominance in streamflow generation: Insights from stable isotopes and tritium tracing in a semi-humid monsoonal catchment Z. Xu et al.
8. 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.
9. Coupling stable isotopes and glacier mass balance reduces uncertainty in glacio-hydrological modelling L. Yong et al.
10. 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.
11. Glaciers determine the sensitivity of hydrological processes to perturbed climate in a large mountainous basin on the Tibetan Plateau Y. Nan & F. Tian
12. Isotope data-constrained hydrological model improves soil moisture simulation and runoff source apportionment Y. Nan & F. Tian
13. Large scale hydrologic and tracer aided modelling: A review T. Stadnyk & T. Holmes
14. Regional contributions of climate change and human activities to altered flow of the Lancang-mekong river K. Zhang et al.
15. Glacier meltwater has limited contributions to the total runoff in the major rivers draining the Tibetan Plateau Y. Nan et al.