Document Type : Original Article
Authors
1
1President Joseph Kasa-Vubu University, Polytechnic Faculty, Boma, Democratic Republic of the Congo 2Regional School of Water (ERE), University of Kinshasa (UNIKIN) and Congo Basin Water Resources Research Center, University of Kinshasa,
2
Regional School of Water (ERE), University of Kinshasa (UNIKIN) and Congo Basin Water Resources Research Center, University of Kinshasa
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Nansen-Tutu Centre for Environmental Marine Research, Department of Oceanography, University of Cape Town,Rondebosch, South Africa and Hydro-Environmental Research Laboratories, Department of Meteorology, Higher Institute of Applied
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Regional School of Water (ERE), University of Kinshasa (UNIKIN) and Congo Basin Water Resources Research Center, University of Kinshasa, Kinshasa, Democratic Republic of the Congo
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University of Quebec in Abitibi-Temiscamingue, School of Engineering, Rouyn-Noranda, Canada
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University of Kinshasa, Faculty of science and technology, Kinshasa and President Joseph Kasa-Vubu University, Polytechnic Faculty, Boma, Democratic Republic of the Congo
10.22044/jhwe.2026.15995.1058
Abstract
Water resources stored in small reservoirs and intake dams are essential for ensuring a reliable water supply, particularly in regions exposed to strong hydroclimatic variability. Climate change and increasing fluctuations in precipitation and evaporation patterns are creating new challenges for the sustainable management of water infrastructures. In Boma, Democratic Republic of the Congo, the Kalamu intake dam experiences recurrent seasonal water shortages due to reduced river discharge during the dry season, reservoir eutrophication, and growing pressure on available water resources. This study aimed to assess the hydroclimatic variability of the Kalamu catchment and evaluate its implications for water availability, reservoir performance, and long-term water resource sustainability. Monthly precipitation and evaporation observations collected at the Boma meteorological station were combined with MERRA-2 reanalysis data covering the period 1992–2023. Statistical analyses, including Pearson correlation, coefficient of determination (R²), Mean Absolute Error (MAE), Root Mean Square Error (RMSE), and bias, were used to evaluate the agreement between observed and reanalysis datasets. Hydroclimatic variability was investigated through water balance analysis, Z-score classification of hydrological years, and trend detection using the Mann–Kendall test and Sen’s slope estimator. The results showed that MERRA-2 satisfactorily reproduced general precipitation patterns but moderately overestimated rainfall and smoothed extreme events. In contrast, evaporation estimates exhibited poor agreement with observations, characterized by a strong negative bias and weak correlation. The hydroclimatic analysis revealed alternating wet and dry years, a cumulative water deficit of 4982.05 m³, and a required storage capacity of 209.88 m³ compared with the current reservoir capacity of only 160 m³. Trend analyses indicated no statistically significant long-term changes in precipitation, evaporation, or water balance, although substantial interannual variability was observed. The study concludes that the Kalamu dam remains vulnerable to seasonal water shortages. Increasing storage capacity, improving reservoir management, strengthening hydroclimatic monitoring, and applying bias correction to reanalysis datasets are recommended to enhance water supply reliability. Furthermore, current hydroclimatic conditions suggest that the installation of a mini-hydropower plant is not presently feasible because water availability remains insufficient to guarantee sustainable energy production without compromising the primary water-supply function of the dam.
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