Introduction
Water is a strategic national asset across all countries, underpinning energy security, agricultural productivity, public safety, and long‑term economic development. In regions characterised by complex terrain, transboundary river basins, and limited monitoring networks, effective water governance depends on the ability to observe, understand, and predict hydrological behaviour. Climate variability and climate change are amplifying extremes, increasing the frequency of both intense precipitation and prolonged droughts. For countries with constrained observational capacity, the combination of exposure and limited monitoring translates directly into higher disaster risk and greater economic volatility. Conversely, many better‑resourced countries have strengthened their water‑information systems by integrating satellite‑based hydrological data, enabling near‑real‑time monitoring of rainfall, soil moisture, snow cover, surface‑water extent, evapotranspiration, and basin‑scale groundwater storage.
Across the six non‑EU Western Balkan states—Albania, Bosnia and Herzegovina, Kosovo, Montenegro, North Macedonia, and Serbia—these pressures are particularly pronounced. Mountainous and karst landscapes, rapid elevation gradients, and highly variable hydrological regimes create conditions where floods, droughts, and groundwater fluctuations can develop quickly. Major river systems such as the Sava, Drina, Morava, Vardar/Axios, and Neretva cross multiple national borders, making transboundary water management an inherent feature of the region’s hydrology. Monitoring networks remain uneven and often too sparse to capture basin‑scale behaviour, limiting the ability to track evolving risks or understand long‑term trends. Satellite‑enabled water intelligence offers a practical and scalable way to address these gaps by providing continuous, independent, basin‑wide visibility that supports real‑time monitoring, early‑warning capability, and evidence‑based planning.
The region’s hydrological vulnerability is shaped not only by physical characteristics but also by institutional and governance arrangements. Fast‑responding catchments heighten flood risk, while seasonal water scarcity and variable groundwater systems place pressure on agriculture, public supply, and energy production. Forecasting systems must operate with limited lead time, and emergency response depends on timely, accurate information that is not always available. Areas influenced by Mediterranean climate patterns and karst hydrology experience pronounced seasonal variability, yet drought monitoring and groundwater assessment remain limited. Transboundary river systems add further complexity, as upstream conditions frequently determine downstream impacts, while monitoring and data systems remain largely national in scope.
Globally, water‑management policy is shifting toward integrated systems that combine ground observations, numerical models, and satellite‑derived datasets. Many countries now treat satellite rainfall, soil moisture, snow cover, evapotranspiration, surface‑water extent, and groundwater storage as essential components of national forecasting and early‑warning architectures. These datasets are openly accessible, consistent across borders, and available even where in‑situ networks are sparse or difficult to maintain. Flood‑forecasting centres assimilate satellite precipitation and soil‑moisture products; drought‑monitoring systems rely on evapotranspiration and vegetation‑stress indicators; and civil‑protection agencies use radar‑based flood mapping to coordinate emergency response. Satellite‑enabled water intelligence has become a standard element of modern hydrological governance.
The non‑EU Western Balkan region has not yet incorporated satellite‑based hydrological information into its operational water‑management systems. Monitoring still relies mainly on conventional observation networks and numerical weather prediction, while satellite datasets are used only intermittently or within short‑term projects. Satellite rainfall data are not routinely assimilated into hydrological models, and soil‑moisture and evapotranspiration data are not part of formal drought‑assessment procedures. Flood‑extent mapping from satellite radar is generally produced only after major events rather than as part of continuous situational awareness. Groundwater‑storage information from international satellite programmes is also absent from planning and policy processes. These gaps reflect institutional fragmentation, uneven investment in monitoring infrastructure, and the lack of a coordinated policy framework. Responsibilities for hydrometeorology, water management, civil protection, and environmental monitoring are spread across multiple agencies, making it difficult to develop shared data pipelines, common modelling platforms, or unified operational procedures. Technical capacity in remote sensing and data assimilation remains limited, and existing IT systems are not designed for high‑volume, near‑real‑time data processing.
Despite these constraints, the region is well positioned to modernise its hydrological information systems. Global satellite missions now provide continuous, open‑access data across all major components of the water cycle, reducing the need for extensive physical monitoring infrastructure. Integrating these datasets into operational workflows would strengthen forecasting capability, improve seasonal outlooks, and enhance long‑term planning. Satellite‑based observation also provides independent visibility across transboundary river systems, enabling authorities to assess upstream conditions without relying solely on bilateral data‑sharing arrangements. Beyond risk reduction, satellite‑enabled water intelligence can support hydropower optimisation, agricultural advisory services, environmental monitoring, and land‑use assessment. Building such a system requires coordinated investment in data management, modelling capacity, and institutional roles, along with a clear policy mandate that recognises satellite hydrology as a strategic capability. With these elements in place, the region can align with international practice and strengthen its resilience to climate‑driven hydrological change.