Rainfall and streamflow variability in North Benin, West Africa, and its multiscale association with climate teleconnections

Three tributaries of the Niger River, covering 48,000 km² in northern Benin, West Africa. Understanding rainfall and streamflow variability in a warming world is crucial for drought-prone West Africa, whose economy relies heavily on rain-fed agriculture. This study explores past changes (1970–2020) in catchment rainfall and streamflow and their association with climate teleconnections. We find consistent rainfall patterns across the three catchments, with a recovery from the 1970s-1980s droughts starting in the 1990s. Total rainfall has increased significantly driven by more rainy days, although the wet day rainfall amount has decreased. These results can be summarized as ‘increased total rainfall, but less intense and more variable in space’. More rain, however, does not mean that the drought situation is alleviated, as high interannual and decadal variability persists. Wavelet coherence reveals that rainfall and streamflow variability are modulated by the climate teleconnections ENSO, AMO, and IOD. For rainfall, we find a tendency of a shift from lower-frequency coherence (4–10 years) in earlier decades to higher-frequency coherence (1–3 years) in recent decades. These patterns are less pronounced for streamflow due to indirect climate influences. Unlike many African studies relying on model simulations, these findings are based on quality-checked, dense station data networks, essential for understanding local climate impacts, water management, and early warning systems. • Consistent rainfall patterns across catchments, with drought recovery starting in the 1990s after severe droughts in the 1970s–1980s. • Total rainfall increased with more rainy days and higher spatial variability more rain overall, but less intense and more unevenly distributed. • Wavelet coherence shows ENSO, AMO, and IOD modulate rainfall-streamflow variability, shifting from 4–10 yr frequency before to 1–3 yr frequency now.

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Publication Details

Journal
Journal of Hydrology Regional Studies
Published
2025-03-22
DOI
https://doi.org/10.1016/j.ejrh.2025.102319
Citations
2
Primary Topic
Hydrology and Drought Analysis
Type
article
Field-Weighted Citation Impact
2.21
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article

Rainfall and streamflow variability in North Benin, West Africa, and its multiscale association with climate teleconnections

Adéchina Eric Alamou, Ezéchiel Obada, Ravi Kumar Guntu, Jean Hounkpè et al.
2 citations
Journal of Hydrology Regional Studies
Hydrology and Drought Analysis
2.21
article

Rainfall and streamflow variability in North Benin, West Africa, and its multiscale association with climate teleconnections

Adéchina Eric Alamou, Ezéchiel Obada, Ravi Kumar Guntu, Jean Hounkpè, Bruno Merz, Kossi François Guedje, Orou Moctar Ganni Mampo, Halissou Yarou
article en
2 citations

Abstract

Three tributaries of the Niger River, covering 48,000 km² in northern Benin, West Africa. Understanding rainfall and streamflow variability in a warming world is crucial for drought-prone West Africa, whose economy relies heavily on rain-fed agriculture. This study explores past changes (1970–2020) in catchment rainfall and streamflow and their association with climate teleconnections. We find consistent rainfall patterns across the three catchments, with a recovery from the 1970s-1980s droughts starting in the 1990s. Total rainfall has increased significantly driven by more rainy days, although the wet day rainfall amount has decreased. These results can be summarized as ‘increased total rainfall, but less intense and more variable in space’. More rain, however, does not mean that the drought situation is alleviated, as high interannual and decadal variability persists. Wavelet coherence reveals that rainfall and streamflow variability are modulated by the climate teleconnections ENSO, AMO, and IOD. For rainfall, we find a tendency of a shift from lower-frequency coherence (4–10 years) in earlier decades to higher-frequency coherence (1–3 years) in recent decades. These patterns are less pronounced for streamflow due to indirect climate influences. Unlike many African studies relying on model simulations, these findings are based on quality-checked, dense station data networks, essential for understanding local climate impacts, water management, and early warning systems. • Consistent rainfall patterns across catchments, with drought recovery starting in the 1990s after severe droughts in the 1970s–1980s. • Total rainfall increased with more rainy days and higher spatial variability more rain overall, but less intense and more unevenly distributed. • Wavelet coherence shows ENSO, AMO, and IOD modulate rainfall-streamflow variability, shifting from 4–10 yr frequency before to 1–3 yr frequency now.

Journal of Hydrology Regional StudiesVol. 59
University of Potsdam (DE), West African Science Service Centre on Climate Change and Adapted Land Use (GH), Université d'Abomey-Calavi (BJ), National University of Sciences, Technologies, Engineering and Mathematics (BJ), GFZ Helmholtz Centre for Geosciences (DE)
Climate action
Openalex Percentile: Top 15%
Hydrology and Drought Analysis
2.21
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