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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 20, issue 1
Hydrol. Earth Syst. Sci., 20, 209–225, 2016
https://doi.org/10.5194/hess-20-209-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 20, 209–225, 2016
https://doi.org/10.5194/hess-20-209-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

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 et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (03 Sep 2015) by Bob Su
AR by Sophie Biskop on behalf of the Authors (13 Oct 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (20 Oct 2015) by Bob Su
RR by Anonymous Referee #2 (29 Oct 2015)
RR by Anonymous Referee #1 (02 Nov 2015)
RR by Anonymous Referee #4 (04 Nov 2015)
ED: Publish subject to minor revisions (Editor review) (13 Nov 2015) by Bob Su
AR by Sophie Biskop on behalf of the Authors (23 Nov 2015)  Author's response    Manuscript
ED: Publish as is (07 Dec 2015) by Bob Su
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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.
In this study, the hydrological model J2000g was extended and applied to four selected endorheic...
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