Multi-decadal dynamics of the Saloum River delta mouth in climate change context. (March 2022)

• Record Type: Journal Article
• Authors: Sadio, M.; Sakho, I.; Samou Seujip, M.; Gueye, A.; Diouf, M.B.; Deloffre, J.
• Is Part Of: Journal of African earth sciences. Volume 187(2022)
• Publication Date: 2022-03
• Subjects: Coastal erosion -- Sandy spit -- Tidal inlet -- Climate change -- Saloum river delta -- Senegal; Earth sciences -- Africa -- Periodicals; Earth sciences -- Middle East -- Periodicals; Geology -- Africa -- Periodicals; Geology -- Middle East -- Periodicals; Sciences de la terre -- Afrique -- Périodiques; Sciences de la terre -- Moyen-Orient -- Périodiques; Géologie -- Afrique -- Périodiques; Géologie -- Moyen-Orient -- Périodiques; Earth sciences; Geology; Africa; Middle East; Periodicals; Electronic journals; 556.05
• DOI: 10.1016/j.jafrearsci.2022.104451
• Languages: English
• ISSNs: 1464-343X

Abstract

Abstract: The coast of Senegal is subject to climate variability that affects coastal dynamics. The Sangomar spit bounding the Saloum River delta provides a striking example. The spit dynamics has been characterized by complex changes involving both erosion and accumulation. Using a methodological approach combining remote sensing and data analysis in a Geographic Information System (GIS) we calculated a mean annual erosion rate of −3.55 m of the spit shoreline from 1954 to 1987. In 1987 the spit was breached by storm in its most eroded sector (- 4.59 m/year). This breach widened significantly to attain 5.25 km in 2018 and has now become the Saloum River mouth. The breach has resulted in exacerbated erosion of adjacent shorelines, especially at the down-drift coast, where the retreat attains a peak of −20.16 m/year, the average erosion rate remaining at −3.56 m/year for the entire coast. Extension of the spit tip has favoured progradation of the Sangomar Pointe which has lengthened by 5.74 km between 1954 and 2018, diverting gradually the Saloum River former mouth towards the South, and corresponding to a 5, 185, 009 m 3 sedimentation. Extrapolation of shoreline mobility reveals high erosion rates due to sea-level rise by 2050 and 2100. Highlights: Sandy spit of the Saloum delta is very vulnerable to coastal erosion. Erosion is greater in the southern part of the mouth compared to the northern part. The southern end of the sandy spit is marked by significant sedimentary accretion, thus forming a barrier island. The opening of the sangomar breach has increased the vulnerability of the saloum delta to the effects of climate change.