Unraveling the hydrology and sediment balance of an ungauged lake in the Sudano-Sahelian region of West Africa using remote sensing

• Published in: Earth surface dynamics 2022-08, Vol.10 (4), p.797-815
• Main Authors: Ragettli, Silvan, Donauer, Tabea, Molnar, Peter, Delnoije, Ron, Siegfried, Tobias
• Format: Article
• Language: English
• Subjects: Arid lands; Arid zones; Bathymetry; Climate change; Dikes (Engineering); Ecological function; Evaporation; Groundwater; Groundwater levels; Groundwater table; Hydrology; Lake beds; Lake shores; Lakes; Land degradation; Levees; Livelihoods; Precipitation; Rainfall; Rainy season; Remote monitoring; Remote sensing; Reservoir capacity; Reservoirs; Runoff; Sea surface; Seasons; Sediment; Sediments; Sediments (Geology); Shoreline protection; Shorelines; Siltation; Silting; Soil erosion; Storage capacity; Storage conditions; Surface water; Tributaries; Unmanned aerial vehicles; Water balance; Water depth; Water levels; Water resources; Water shortages; Water table; Watersheds; Wet season
• ISSN: 2196-632X; 2196-6311; 2196-632X
• DOI: 10.5194/esurf-10-797-2022

The presence of ephemeral ponds and perennial lakes in the Sudano-Sahelian region of West Africa is strongly variable in space and time. Yet, they have important ecological functions and societies are reliant on their surface waters for their lives and livelihoods. It is essential to monitor and understand the dynamics of these lakes to assess past, present, and future water resource changes. In this paper, we present an innovative approach to unravel the sediment and water balance of Lac Wégnia, a small ungauged lake in Mali near the capital of Bamako. The approach uses optical remote sensing data to identify the shoreline positions over a period of 22 years (2000–2021) and then attributes water surface heights (WSHs) to each observation using the lake bathymetry. We then present a novel methodology to identify and quantitatively analyze deposition and erosion patterns at lakeshores and in lake beds. The method therefore represents a significant advancement over previous attempts to remotely monitor lakes in the West African drylands, since it considers not only changes in water depth to explain recent declining trends in lake areas, but also changes in the storage capacity. At Lac Wégnia, we recognize silting at the tributaries to the lake, but overall, erosion processes are dominant and threaten the persistence of the lake because of progressive erosion through the natural levee at the lake outlet. This factor contributes 66 %±18 % to the decreasing WSH trend, while 34 %±18 % of the dry-season lake level changes are explained by increasing evaporation from the lake and by possibly falling groundwater tables. Due to the decreasing reservoir capacity of the lake, WSHs are declining even in the wet season in spite of positive rainfall patterns.