Articles | Volume 25, issue 12
https://doi.org/10.5194/hess-25-6151-2021
https://doi.org/10.5194/hess-25-6151-2021
Research article
 | 
03 Dec 2021
Research article |  | 03 Dec 2021

Can we use precipitation isotope outputs of isotopic general circulation models to improve hydrological modeling in large mountainous catchments on the Tibetan Plateau?

Yi Nan, Zhihua He, Fuqiang Tian, Zhongwang Wei, and Lide Tian

Viewed

Total article views: 2,596 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,860 686 50 2,596 25 33
  • HTML: 1,860
  • PDF: 686
  • XML: 50
  • Total: 2,596
  • BibTeX: 25
  • EndNote: 33
Views and downloads (calculated since 28 May 2021)
Cumulative views and downloads (calculated since 28 May 2021)

Viewed (geographical distribution)

Total article views: 2,596 (including HTML, PDF, and XML) Thereof 2,445 with geography defined and 151 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 28 Mar 2024
Download
Short summary
Hydrological modeling has large problems of uncertainty in cold regions. Tracer-aided hydrological models are increasingly used to reduce uncertainty and refine the parameterizations of hydrological processes, with limited application in large basins due to the unavailability of spatially distributed precipitation isotopes. This study explored the utility of isotopic general circulation models in driving a tracer-aided hydrological model in a large basin on the Tibetan Plateau.