%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Brempong, E. K.
%A Almar, Rafaël
%A Angnuureng, D. B.
%A Mattah, P. A. D.
%A Jayson-Quashigah, P. N.
%A Antwi-Agyakwa, K. T.
%A Charuka, B.
%T Coastal flooding caused by extreme coastal water level at the world heritage historic Keta City (Ghana, West Africa)
%D 2023
%L fdi:010088205
%G ENG
%J Journal of Marine Science and Engineering
%K Gulf of Guinea ; wave run-up ; sea level rise ; coastal flooding
%K GHANA ; GOLFE DE GUINEE ; VOLGA DELTA
%M ISI:001017271500001
%N 6
%P 1144 [18 ]
%R 10.3390/jmse11061144
%U https://www.documentation.ird.fr/hor/fdi:010088205
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2023-08/010088205.pdf
%V 11
%W Horizon (IRD)
%X Like low-lying sandy coasts around the world, the Ghanaian coast is experiencing increasingly frequent coastal flooding due to climate change, putting important socioeconomic infrastructure and people at risk. Our study assesses the major factors contributing to extreme coastal water levels (ECWLs) from 1994 to 2015. ECWLs are categorized into low, moderate, and severe levels corresponding to the 30th, 60th, and 98th percentiles, respectively. Using these three levels over the Pleiades satellite-derived digital elevation model topography, potential flood extent zones are mapped. ECWLs have the potential to flood more than 40% of the study area, including socioeconomically important sites such as tourist beach resorts, Cape St. Paul lighthouse, and Fort Prinzenstein. In this study, all coastal flooding events recorded by the municipality of Keta fall within the 98th percentile category. Our results show a gradual increase in the frequency of flooding over the years. Flooding events are caused by a compound effect of the tide, sea level anomaly, waves, and atmospheric conditions. Finally, while wave run-up is the major contributor to coastal flooding, the tide is the one varying most, which facilitates a simple early warning system based on waves and tide but adds uncertainty and complicates long-term predictability.
%$ 062 ; 032 ; 102