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

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

doi:10.5194/hess-20-209-2016

Articles | Volume 20, issue 1

https://doi.org/10.5194/hess-20-209-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/hess-20-209-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 20, issue 1

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

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Jan 2026	111	34	9	154
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Cumulative views and downloads (calculated since 29 Apr 2015)

Month	HTML	PDF	XML	Total
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May 2015	33	49	2	84
Jun 2015	18	15	0	33
Jul 2015	18	43	1	62
Aug 2015	16	48	1	65
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Nov 2015	17	12	1	30
Dec 2015	9	17	1	27
Jan 2016	103	41	3	147
Feb 2016	53	47	3	103
Mar 2016	47	29	16	92
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Latest update: 12 Apr 2026

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.