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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 5
Hydrol. Earth Syst. Sci., 17, 1985–2000, 2013
https://doi.org/10.5194/hess-17-1985-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 17, 1985–2000, 2013
https://doi.org/10.5194/hess-17-1985-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 May 2013

Research article | 27 May 2013

Analysis of long-term terrestrial water storage variations in the Yangtze River basin

Y. Huang1,2, M. S. Salama1, M. S. Krol2, R. van der Velde1, A. Y. Hoekstra2, Y. Zhou3, and Z. Su1 Y. Huang et al.
  • 1Faculty of Geo-Information Science and Earth Observation (ITC), Department of Water Resources, University of Twente, Enschede, the Netherlands
  • 2Faculty of Engineering Technology, Department of Water Engineering and Management (WEM), University of Twente, Enschede, the Netherlands
  • 3State Key Lab of Estuarine and Coastal Research (SKLEC), East China Normal University, Shanghai, P.R. China

Abstract. In this study, we analyze 32 yr of terrestrial water storage (TWS) data obtained from the Interim Reanalysis Data (ERA-Interim) and Noah model from the Global Land Data Assimilation System (GLDAS-Noah) for the period 1979 to 2010. The accuracy of these datasets is validated using 26 yr (1979–2004) of runoff data from the Yichang gauging station and comparing them with 32 yr of independent precipitation data obtained from the Global Precipitation Climatology Centre Full Data Reanalysis Version 6 (GPCC) and NOAA's PRECipitation REConstruction over Land (PREC/L). Spatial and temporal analysis of the TWS data shows that TWS in the Yangtze River basin has decreased significantly since the year 1998. The driest period in the basin occurred between 2005 and 2010, and particularly in the middle and lower Yangtze reaches. The TWS figures changed abruptly to persistently high negative anomalies in the middle and lower Yangtze reaches in 2004. The year 2006 is identified as major inflection point, at which the system starts exhibiting a persistent decrease in TWS. Comparing these TWS trends with independent precipitation datasets shows that the recent decrease in TWS can be attributed mainly to a decrease in the amount of precipitation. Our findings are based on observations and modeling datasets and confirm previous results based on gauging station datasets.

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