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.
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.
the Creative Commons Attribution 3.0 License.
Differences in the water-balance components of four lakes in the southern-central Tibetan Plateau
S. Biskop
CORRESPONDING AUTHOR
Department of Geography, Friedrich Schiller University
Jena, Germany
F. Maussion
Institute of Atmospheric and Cryospheric Sciences, University of
Innsbruck, Austria
P. Krause
Thuringian State Institute for Environment and Geology,
Jena, Germany
Department of Geography, Friedrich Schiller University
Jena, Germany
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4 citations as recorded by crossref.
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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...