Abstract
Water storage change has implications not only for the hydrological cycle, but also for sustainable water resource management in especially semi-arid river basins. Satellite/remote sensing techniques have gained increasing application in monitoring basin and regional hydrological processes in recent decades. In this study, the latest version of GRACE (Gravity Recovery and Climate Experiment) is used to estimate total water storage change in the Hai River basin (HRB) of Northern China for the period January 2003 to December 2006. Time-series comparisons show a good agreement between the estimated storage change from the GRACE satellite data and in situ hydrological measurement data at especially the seasonal cycle with R = 0.82 and RMSE = 17.25 mm. The good agreement suggests that GRACE detects storage change in the 318 866 km2 HRB study area. It also implies that the in situ hydrological measurements of soil moisture and groundwater sufficiently characterise storage change in the semi-arid river basin. Change in soil moisture storage is less than that insaturated storage, suggesting that storage depletion in the basin is mainly in the saturated zone. Both the GRACE and hydrological measurement data indicate storage loss in the range of 12.72 to 23.76 mm/yr – a phenomenon that has been detected in previous studies in the basin. GRACE hydrology data could therefore be handy in monitoring storage dynamics and water availability in the study area. As GRACE data are available for virtually every region of the world, their application in conjunction with hydrological models could improve hydrological studies. This may lead not only to water balance closures, but also to sustainable water resource management at basin to regional scale.
Highlights
Water shortage on North China Plain (NCP), the largest wheat/ maize production zone in China, is a limiting factor to socioeconomic development in the region (Guobin et al, 2004; Yang et al, 2006)
Total water storage change in Hai River basin was successfully estimated for the period January 2003 to December 2006 using GRACE and in situ hydrological measurement data
Total water storage derived from GRACE data was compared with that computed from in situ hydrological measurement data of soil moisture and groundwater
Summary
Water shortage on North China Plain (NCP), the largest wheat/ maize production zone in China, is a limiting factor to socioeconomic development in the region (Guobin et al, 2004; Yang et al, 2006). GRACE and the combined hydrological measurement data of soil moisture and groundwater were used to analyze total water storage change in the 318 866 km Hai River basin (HRB). The basin-averaged monthly storage anomaly was afterwards derived from the raster maps after re-truncation to the study area This processing technique was necessary because the spatial extent of HRB defined in our study (see Fig. 1) is essentially different from that on the GRACE website – where the basin definitions are based on TRIP (Total Runoff Integrating Pathways; see Oki and Sud (1998)). For the purpose of this study, all measurement sites with standard mean relative difference deviation above the average mean (5.20 mm for the soil moisture and 5.07 m for the water table data) were considered outliers and were rejected. The terms on the opposite sides of the equation should be commensurate and comparable
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