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The hydrological regimes of the Upper Blue Nile Basin (UBNB) are undergoing rapid transformation under the combined influence of climate change and land use/land cover dynamics. This review aims to synthesize the hydrological responses of the UBNB to projected climate change and land use/land cover alteration, both in isolation and in combination. The reviewed studies span different sub-basins, watersheds, climate scenarios, modelling approaches, and future time horizons, resulting in considerable variability in reported hydrological responses. Nevertheless, study-specific projections in the UBNB indicate future reductions in dry-season flow of approximately 35-50% under specific climate scenarios and future periods, alongside increases in wet-season peak flows. Land use/land cover change alone is associated with a projected 5–24% future increase in Surface Runoff (SR) and reduced baseflow based on the reviewed studies. The combined effects of climate change and land use/land cover are generally more pronounced than their isolated impacts, resulting in a more runoff-dominated hydrological regime. Across the reviewed studies in the UBNB, the combined effects are reported to result in a future increase in water yield (up to 30.4%), SR (up to 27.8%), sediment yield (up to 41.01%), and a decline in groundwater flow (up to 15.30%). The findings highlight the need for proactive and integrated watershed management, including sustainable land-use planning, soil and water conservation, reforestation, and climate-resilient infrastructure to safeguard water security in the UBNB. They also emphasize the importance of considering both climate change and land use/land cover impacts in water resource planning. Future research should reduce model uncertainties and use downscaled Global Climate Model data to guide site-specific adaptive strategies.
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Atlaw et al. (2026) studied this question.
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