Spatiotemporal Dynamics of Drought in the Huai River Basin (2012–2018): Analyzing Patterns Through Hydrological Simulation and Geospatial Methods

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Abstract
As climate change intensifies, extreme drought events have become more frequent, and investigating the mechanisms of watershed drought has become highly significant for basin water resource management. This study utilizes the WRF-Hydro model in conjunction with standardized drought indices, including the standardized precipitation index (SPI), standardized soil moisture index (SSMI), and Standardized Streamflow Index (SSFI), to comprehensively investigate the spatiotemporal characteristics of drought in the Huai River Basin, China, from 2012 to 2018. The simulation performance of the WRF-Hydro model was evaluated by comparing model outputs with reanalysis data at the regional scale and site observational data at the site scale, respectively. Our results demonstrate that the model showed a correlation coefficient of 0.74, a bias of −0.29, and a root mean square error of 2.66% when compared with reanalysis data in the 0–10 cm soil layer. Against the six observational sites, the model achieved a maximum correlation coefficient of 0.81, a minimum bias of −0.54, and a minimum root mean square error of 3.12%. The simulation results at both regional and site scales demonstrate that the model achieves high accuracy in simulating soil moisture in this basin. The analysis of SPI, SSMI, and SSFI from 2012 to 2018 shows that the summer months rarely experience drought, and droughts predominantly occurred in December, January, and February in the Huai River Basin. Moreover, we found that the drought characteristics in this basin have significant seasonal and interannual variability and spatial heterogeneity. On the one hand, the middle and southern parts of the basin experience more frequent and severe agricultural droughts compared to the northern regions. On the other hand, we identified a time–lag relationship among meteorological, agricultural, and hydrological droughts, uncovering interactions and propagation mechanisms across different drought types in this basin. Finally, we concluded that the WRF-Hydro model can provide highly accurate soil moisture simulation results and can be used to assess the spatiotemporal variations in regional drought events and the propagation mechanisms between different types of droughts.
Funding Information
  • National Natural Science Foundation of China (42101361, 2024M753092, 2022m07020003, 2408055UQ006, 2023AH050143, 202310370056, 202310370051)
  • China Postdoctoral Science Foundation (42101361, 2024M753092, 2022m07020003, 2408055UQ006, 2023AH050143, 202310370056, 202310370051)
  • Key Research and Development Program of Anhui (42101361, 2024M753092, 2022m07020003, 2408055UQ006, 2023AH050143, 202310370056, 202310370051)
  • Jianghuai Meteorological Joint Project of Anhui Natural Science Foundation (42101361, 2024M753092, 2022m07020003, 2408055UQ006, 2023AH050143, 202310370056, 202310370051)
  • Scientific Research Project of Higher Education Institutions in Anhui Province (42101361, 2024M753092, 2022m07020003, 2408055UQ006, 2023AH050143, 202310370056, 202310370051)
  • National Undergraduate Innovation and Entrepreneurship Training Program (42101361, 2024M753092, 2022m07020003, 2408055UQ006, 2023AH050143, 202310370056, 202310370051)

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