Abstract
Ongoing socio-economic developments and climatic change have been pressurizing the groundwater resource availability in the Abaya–Chamo lakes basin, Ethiopian Rift valley. The primary goals of the present study are: (1) to simulate the groundwater gradient and flow direction, (2) to calculate the groundwater balances and flux of the sub-major river basins under the water budget code of the MODFLOW, and (3) to predict the future groundwater levels of the lake's basin under a projected changing climate. The numerical groundwater flow of the Abaya–Chamo lakes basin aquifer system is simulated using the USGS three-dimensional finite-difference groundwater flow model MODFLOW-2005 with Block centered flow packages (BCF). The following datasets, such as aquifer properties, geology, recharge, discharge, topography, etc., were used to simulate the present model. The calibrated steady-state groundwater flow modeling simulation of the Abaya–Chamo lakes basin also confirmed the through-flow system in terms of groundwater gradient and flow direction, on which groundwater flow happens from the plateau toward the floor into the lakes from both directions with a high gradient exist in the escarpment. The present study provides a sound foundation for modern scientific direction in water resource evaluation by establishing integrated surface and groundwater models that change climatic conditions for sustainable water resources management.
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Acknowledgements
The authors are grateful to the School of Earth Sciences, Addis Ababa University and Faculty of Meteorology and Hydrology, Water Technology Institute, Arba Minch University, Ethiopia for the support of the research. Additionally, we are thankful to the National Meteorological Agency, Ministry of Water Irrigation, Electricity, and Geological Survey of Ethiopia for providing relevant data.
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Daniel, D., Ayenew, T., Fletcher, C.G. et al. Numerical groundwater flow modelling under changing climate in Abaya–Chamo lakes basin, Rift Valley, Southern Ethiopia. Model. Earth Syst. Environ. 8, 3985–3999 (2022). https://doi.org/10.1007/s40808-021-01342-x
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DOI: https://doi.org/10.1007/s40808-021-01342-x