Articles | Volume 25, issue 6
https://doi.org/10.5194/hess-25-3653-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-3653-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
30 Jun 2021
Research article |
| 30 Jun 2021
| 30 Jun 2021
The value of water isotope data on improving process understanding in a glacierized catchment on the Tibetan Plateau
Department of Hydraulic Engineering, State Key Laboratory of
Hydroscience and Engineering, Tsinghua University, Beijing 100084, China
Lide Tian
Institute of International Rivers and Eco-security, Yunnan University, Kunming, China
Center of Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China
Zhihua He
Center for Hydrology, University of Saskatchewan, Saskatchewan, Canada
Department of Hydraulic Engineering, State Key Laboratory of
Hydroscience and Engineering, Tsinghua University, Beijing 100084, China
Lili Shao
Institute of International Rivers and Eco-security, Yunnan University, Kunming, China
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Cited
21 citations as recorded by crossref.
- Assessing the influence of water sampling strategy on the performance of tracer-aided hydrological modeling in a mountainous basin on the Tibetan Plateau Y. Nan et al. 10.5194/hess-26-4147-2022
- Upscaling Tracer‐Aided Ecohydrological Modeling to Larger Catchments: Implications for Process Representation and Heterogeneity in Landscape Organization X. Yang et al. 10.1029/2022WR033033
- Synoptic water isotope surveys to understand the hydrology of large intensively managed catchments K. Chen et al. 10.1016/j.jhydrol.2023.129817
- 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
- Evaluating input data sources for isotope‐enabled rainfall‐runoff models A. Watson et al. 10.1002/hyp.15276
- Temperature and precipitation control the seasonal patterns of discharge and water isotopic signals of the Nyang River on the southeastern Tibetan Plateau W. Ren et al. 10.1016/j.jhydrol.2023.129064
- Guidance on large scale hydrologic model calibration with isotope tracers T. Holmes et al. 10.1016/j.jhydrol.2023.129604
- Effects of passive-storage conceptualization on modeling hydrological function and isotope dynamics in the flow system of a cockpit karst landscape G. Li et al. 10.5194/hess-26-5515-2022
- 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
- Can we use precipitation isotope outputs of isotopic general circulation models to improve hydrological modeling in large mountainous catchments on the Tibetan Plateau? Y. Nan et al. 10.5194/hess-25-6151-2021
- THE INFLUENCE OF VARIATION IN ALTITUDE ON ATHLETIC PERFORMANCE IN LONG-DISTANCE RUNNERS S. Wang et al. 10.1590/1517-8692202228052022_0101
- Altitude effect of precipitation isotopes in an arid mountain-basin system: Observation and modelling around the world’s second-largest shifting desert S. Wang et al. 10.1016/j.jhydrol.2024.131351
- Are temporary stream observations useful for calibrating a lumped hydrological model? M. Scheller et al. 10.1016/j.jhydrol.2024.130686
- The Evaporation on the Tibetan Plateau Stops Increasing in the Recent Two Decades L. Wang et al. 10.1029/2022JD037377
- Spatiotemporal responses of runoff to climate change in the southern Tibetan Plateau H. Sun et al. 10.5194/hess-28-4361-2024
- Large scale hydrologic and tracer aided modelling: A review T. Stadnyk & T. Holmes 10.1016/j.jhydrol.2023.129177
- On the cause of large daily river flow fluctuations in the Mekong River K. Morovati et al. 10.5194/hess-28-5133-2024
- 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
- Isotope data-constrained hydrological model improves soil moisture simulation and runoff source apportionment Y. Nan & F. Tian 10.1016/j.jhydrol.2024.131006
- Non-monotonic changes in Asian Water Towers’ streamflow at increasing warming levels T. Cui et al. 10.1038/s41467-023-36804-6
- Characteristics and Attribution of Spatiotemporal Changes in Qilian Mountains' Runoff Over the Past Six Decades Z. Liu et al. 10.1029/2023JD039176
21 citations as recorded by crossref.
- Assessing the influence of water sampling strategy on the performance of tracer-aided hydrological modeling in a mountainous basin on the Tibetan Plateau Y. Nan et al. 10.5194/hess-26-4147-2022
- Upscaling Tracer‐Aided Ecohydrological Modeling to Larger Catchments: Implications for Process Representation and Heterogeneity in Landscape Organization X. Yang et al. 10.1029/2022WR033033
- Synoptic water isotope surveys to understand the hydrology of large intensively managed catchments K. Chen et al. 10.1016/j.jhydrol.2023.129817
- 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
- Evaluating input data sources for isotope‐enabled rainfall‐runoff models A. Watson et al. 10.1002/hyp.15276
- Temperature and precipitation control the seasonal patterns of discharge and water isotopic signals of the Nyang River on the southeastern Tibetan Plateau W. Ren et al. 10.1016/j.jhydrol.2023.129064
- Guidance on large scale hydrologic model calibration with isotope tracers T. Holmes et al. 10.1016/j.jhydrol.2023.129604
- Effects of passive-storage conceptualization on modeling hydrological function and isotope dynamics in the flow system of a cockpit karst landscape G. Li et al. 10.5194/hess-26-5515-2022
- 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
- Can we use precipitation isotope outputs of isotopic general circulation models to improve hydrological modeling in large mountainous catchments on the Tibetan Plateau? Y. Nan et al. 10.5194/hess-25-6151-2021
- THE INFLUENCE OF VARIATION IN ALTITUDE ON ATHLETIC PERFORMANCE IN LONG-DISTANCE RUNNERS S. Wang et al. 10.1590/1517-8692202228052022_0101
- Altitude effect of precipitation isotopes in an arid mountain-basin system: Observation and modelling around the world’s second-largest shifting desert S. Wang et al. 10.1016/j.jhydrol.2024.131351
- Are temporary stream observations useful for calibrating a lumped hydrological model? M. Scheller et al. 10.1016/j.jhydrol.2024.130686
- The Evaporation on the Tibetan Plateau Stops Increasing in the Recent Two Decades L. Wang et al. 10.1029/2022JD037377
- Spatiotemporal responses of runoff to climate change in the southern Tibetan Plateau H. Sun et al. 10.5194/hess-28-4361-2024
- Large scale hydrologic and tracer aided modelling: A review T. Stadnyk & T. Holmes 10.1016/j.jhydrol.2023.129177
- On the cause of large daily river flow fluctuations in the Mekong River K. Morovati et al. 10.5194/hess-28-5133-2024
- 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
- Isotope data-constrained hydrological model improves soil moisture simulation and runoff source apportionment Y. Nan & F. Tian 10.1016/j.jhydrol.2024.131006
- Non-monotonic changes in Asian Water Towers’ streamflow at increasing warming levels T. Cui et al. 10.1038/s41467-023-36804-6
- Characteristics and Attribution of Spatiotemporal Changes in Qilian Mountains' Runoff Over the Past Six Decades Z. Liu et al. 10.1029/2023JD039176
Latest update: 17 Jan 2025
Short summary
This study integrated a water isotope module into the hydrological model THREW. The isotope-aided model was subsequently applied for process understanding in the glacierized watershed of Karuxung river on the Tibetan Plateau. The model was used to quantify the contribution of runoff component and estimate the water travel time in the catchment. Model uncertainties were significantly constrained by using additional isotopic data, improving the process understanding in the catchment.
This study integrated a water isotope module into the hydrological model THREW. The...
