Growth in Agricultural Water Demand Aggravates Water Supply-Demand Risk in Arid Northwest China: More a result of Anthropogenic Activities than Climate Change
Abstract. Maintaining regional water supply-demand balance is crucial for achieving sustainable development. Although the impacts of climate change and anthropogenic activities on water resources are widely recognized, the dynamic response mechanisms of water supply-demand risk (WSDR) under their combined forcing remain unclear. The Tailan River Basin (TRB), though situated in a typical arid climate zone, serves as China's vital fruit and high-quality grain production base due to abundant solar-thermal resources. However, systematic research on WSDR in this region is deficient, impeding guidance for healthy and stable development of large-scale farming. To address this, we developed a WSDR analytical framework based on PLUS-InVEST models, encompassing 24 climate-land change scenarios. This framework quantifies impacts of climate change and anthropogenic activities on TRB's water supply-demand patterns and associated risks. Results show that under the Balanced Economy-Ecology Strategy (BES), effective land consolidation could add 531.2 km² of cultivated land by 2050. However, significant cultivated land expansion drives minimum water demand to surge to 4.87×10⁸ m³, while maximum regional water supply reaches only 0.16×10⁸ m³, breaking the supply-demand balance. By 2050, the entire TRB will face WSDR crises, with at least 46 % of the region enduring endangered (Level Ⅲ) risk. The root cause is persistent anthropogenic activities-particularly land-use change-triggering continuous cultivated land expansion, increasing irrigation water demand and intensifying conflicts between water demand and supply capacity. These findings underscore the need to deeply integrate multidisciplinary approaches within WSDR frameworks, in-depth analysis of land-ecology-hydrology feedback mechanisms, to better address water security challenges under climate change. This study can provide an important scientific basis for the optimal allocation of regional soil and water resources and the sustainable development of agroecology.