Abstract
Terrestrial water storage changes (TWSCs) retrieved from the Gravity Recovery and Climate Experiment (GRACE) satellite mission have been extensively evaluated in previous studies over large basin scales. However, monitoring the TWSC at small basin scales is still poorly understood. This study presented a new method for calculating TWSCs at the small basin scales based on the water balance equation, using hydrometeorological and multi-source data. First, the basin was divided into several sub-basins through the slope runoff simulation algorithm. Secondly, we simulated the evapotranspiration (ET) and outbound runoff of each sub-basin using the PML_V2 and SWAT. Lastly, through the water balance equation, the TWSC of each sub-basin was obtained. Based on the estimated results, we analyzed the temporal and spatial variations in precipitation, ET, outbound runoff, and TWSC in the Ganjiang River Basin (GRB) from 2002 to 2018. The results showed that by comparing with GRACE products, in situ groundwater levels data, and soil moisture storage, the TWSC calculated by this study is in good agreement with these three data. During the study period, the spatial and temporal variations in precipitation and runoff in the GRB were similar, with a minimum in 2011 and maximum in 2016. The annual ET changed gently, while the TWSC fluctuated greatly. The findings of this study could provide some new information for improving the estimate of the TWSC at small basin scales.
Highlights
Published: 20 August 2021Terrestrial water storage (TWS) is the sum of all forms of water storage over land surfaces and plays a vital role in the global and regional hydrological cycle [1,2,3]
Numerous studies have shown that Gravity Recovery and Climate Experiment (GRACE) satellites play a key role in the large-scale monitoring of Terrestrial water storage changes (TWSCs) or TWS anomalies (TWSA) [8,9,10]
The small-scale basin division results of the Ganjiang River Basin (GRB) can be divided into two levels
Summary
Terrestrial water storage (TWS) is the sum of all forms of water storage over land surfaces and plays a vital role in the global and regional hydrological cycle [1,2,3]. It reflects all types of water stored on continents, including surface water, soil water, and groundwater [4]. The launch of the Gravity Recovery and Climate Experiment (GRACE) satellites has provided a new method for terrestrial hydrology research, which can efficiently improve the monitoring result of the changes in the water cycle at a large scale [7].
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
