Wang Junde, Zhou Wan, Liu Dedi, Cheng Yufei
Gansu Academy for Water Conservancy, Lanzhou, China.
State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, China; Department of Geography, The University of Hong Kong, Hong Kong SAR, China.
J Environ Manage. 2025 Aug;389:126101. doi: 10.1016/j.jenvman.2025.126101. Epub 2025 Jun 9.
Droughts are the most widespread natural disasters in arid/semi-arid regions, causing significant damage to socio-economic and agricultural systems. Inter-basin water diversion projects have been widely adopted to mitigate regional water scarcity. However, the dual impact of drought and water diversion on both water donating and receiving regions remains insufficiently explored. This study investigates the spatiotemporal evolution and risk of hydrological drought (HD) in the context of the Tao River Water Diversion Project (TRWDP) in Gansu province, China. By integrating hydro-meteorological datasets, SWAT-based hydrological modeling, and the Standardized Runoff Index (SRI), HD dynamics were assessed across both water-donating (TRB) and water-receiving regions (ZRB and WRB) from 1970 to 2020. Results indicate that: (1) HD exhibits a worsening trend, with the most pronounced intensification observed in the WRB. (2) Correlation analyses indicate that drought characteristics are driven by diverse climatic and catchment attributes. In the TRB, HD is primarily influenced by seasonal drought index, elevation variability, and proportion of water bodies; in the ZRB, by basin area, river network length, maximum elevation, and forest coverage; and in the WRB, by minimum elevation, river network density, and water area ratio. (3) A risk assessment framework integrating hazard, exposure, and vulnerability highlights critical drought hotspots in the lower TRB and central WRB. Notably, the implementation of the TRWDP has significantly alleviated drought risk in water-receiving regions, particularly in agricultural and densely populated areas. However, the potential redistribution of drought pressure toward water-donating regions underscores the need for balanced inter-basin water governance. These findings bridge the gap in understanding the interplay between water diversion and hydrological drought risk, providing a scientific basis for the adaptive management and sustainable operation of large-scale water transfer projects under climate variability.
干旱是干旱/半干旱地区最普遍的自然灾害,对社会经济和农业系统造成重大破坏。跨流域调水工程已被广泛采用,以缓解区域水资源短缺问题。然而,干旱和调水对供水区和受水区的双重影响仍未得到充分研究。本研究调查了中国甘肃省洮河调水工程(TRWDP)背景下水文干旱(HD)的时空演变和风险。通过整合水文气象数据集、基于SWAT的水文模型和标准化径流指数(SRI),评估了1970年至2020年供水区(洮河流域,TRB)和受水区(漳河流域,ZRB和渭河流域,WRB)的HD动态。结果表明:(1)HD呈恶化趋势,在WRB中加剧最为明显。(2)相关分析表明,干旱特征受多种气候和集水区属性驱动。在TRB中,HD主要受季节干旱指数、海拔变异性和水体比例影响;在ZRB中,受流域面积、河网长度、最大海拔和森林覆盖率影响;在WRB中,受最低海拔、河网密度和水域面积比影响。(3)一个整合了灾害、暴露和脆弱性的风险评估框架突出了TRB下游和WRB中部的关键干旱热点地区。值得注意的是,TRWDP的实施显著缓解了受水区的干旱风险,特别是在农业和人口密集地区。然而,干旱压力可能会重新分配到供水区,这凸显了平衡跨流域水资源治理的必要性。这些发现填补了对调水与水文干旱风险之间相互作用理解的空白,为气候变化下大型调水工程的适应性管理和可持续运行提供了科学依据。