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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 10
Hydrol. Earth Syst. Sci., 17, 3759–3778, 2013
https://doi.org/10.5194/hess-17-3759-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 17, 3759–3778, 2013
https://doi.org/10.5194/hess-17-3759-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 02 Oct 2013

Research article | 02 Oct 2013

Integrated hydrological modeling of the North China Plain and implications for sustainable water management

H. Qin1, G. Cao1, M. Kristensen2, J. C. Refsgaard3, M. O. Rasmussen4, X. He3, J. Liu1, Y. Shu5, and C. Zheng1,6 H. Qin et al.
  • 1Center for Water Research, College of Engineering, Peking University, Beijing 100871, China
  • 2ALECTIA, Teknikerbyen 34, 2830 Virum, Denmark
  • 3Geological Survey of Denmark and Greenland (GEUS), 1350 Copenhagen, Denmark
  • 4DHI GRAS A/S, Oester Voldgade 10, 1350 Copenhagen K, Denmark
  • 5International Water Management Institute Southern African Office, 141 Cresswell Road, Pretoria, 0184, South Africa
  • 6Department of Geological Sciences, University of Alabama, Tuscaloosa, AL 35487, USA

Abstract. Groundwater overdraft has caused fast water level decline in the North China Plain (NCP) since the 1980s. Although many hydrological models have been developed for the NCP in the past few decades, most of them deal only with the groundwater component or only at local scales. In the present study, a coupled surface water–groundwater model using the MIKE SHE code has been developed for the entire alluvial plain of the NCP. All the major processes in the land phase of the hydrological cycle are considered in the integrated modeling approach. The most important parameters of the model are first identified by a sensitivity analysis process and then calibrated for the period 2000–2005. The calibrated model is validated for the period 2006–2008 against daily observations of groundwater heads. The simulation results compare well with the observations where acceptable values of root mean square error (RMSE) (most values lie below 4 m) and correlation coefficient (R) (0.36–0.97) are obtained. The simulated evapotranspiration (ET) is then compared with the remote sensing (RS)-based ET data to further validate the model simulation. The comparison result with a R2 value of 0.93 between the monthly averaged values of simulated actual evapotranspiration (AET) and RS AET for the entire NCP shows a good performance of the model. The water balance results indicate that more than 70% of water leaving the flow system is attributed to the ET component, of which about 0.25% is taken from the saturated zone (SZ); about 29% comes from pumping, including irrigation pumping and non-irrigation pumping (net pumping). Sustainable water management analysis of the NCP is conducted using the simulation results obtained from the integrated model. An effective approach to improve water use efficiency in the NCP is by reducing the actual ET, e.g. by introducing water-saving technologies and changes in cropping.

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