Background
The study area in the Middle East comprises the territories of Israel, Jordan and the Palestinian Territories of the West Bank. The entire region is subjected to enormous water stress and political tensions, because its scarce water resources are jointly managed by Israel, Palestine and Jordan, whose management strategies also require cooperation and joint approaches to solutions.
The target region is also characterized by high hydrological variability and evaporation losses, i.e. strongly fluctuating availability of surface and groundwater and consequently an overuse of groundwater resources, insufficient wastewater treatment and thus water contamination, as well as constant growth of industry and population.
The GRaCCE project aims at the development of a process-based integrated method to determine groundwater recharge and predict droughts in order to support water management in semi-arid regions such as Israel, Palestine and Jordan. Porous-fractured bedrock aquifers contain important groundwater resources and, due to their heterogeneous structure, require adapted assessment and modeling methods to capture the highly dynamic and often difficult-to-predict infiltration rates. Previous studies show that the thick vadose zones (several hundreds of meter) prevalent in the region can be relevant for water management as long-term reservoirs and, if properly considered as a dynamic water resource, can contribute to mitigating supply shortages during long-term droughts. Due to the dual permeability characteristics of the vadose zone in fracture and karst aquifer systems, i.e., fast and slow pathways and their interaction, quantification of water fluxes through the unsaturated zone requires additional scientific effort.