Articles | Volume 20, issue 1
https://doi.org/10.5194/hess-20-209-2016
https://doi.org/10.5194/hess-20-209-2016
Research article
 | 
18 Jan 2016
Research article |  | 18 Jan 2016

Differences in the water-balance components of four lakes in the southern-central Tibetan Plateau

S. Biskop, F. Maussion, P. Krause, and M. Fink

Viewed

Total article views: 5,097 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,705 2,193 199 5,097 561 127 165
  • HTML: 2,705
  • PDF: 2,193
  • XML: 199
  • Total: 5,097
  • Supplement: 561
  • BibTeX: 127
  • EndNote: 165
Views and downloads (calculated since 29 Apr 2015)
Cumulative views and downloads (calculated since 29 Apr 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 21 Nov 2024
Download
Short summary
In this study, the hydrological model J2000g was extended and applied to four selected endorheic lake basins in the southern-central part of the TP aiming to provide a more quantitative understanding of the key factors controlling their water balance. The model results indicated that the relative contribution of glacier runoff to total water inflow (between 14 and 30 %) plays a less important role compared to runoff generation from rainfall and snowmelt in non-glacierized land areas.