Article
Response of the barrier island coastal region of southwestern Nigeria to climate and non-climate forcing
DOI:
10.2989/1814232X.2020.1727953
Author(s):
IB Danladi Department of Geological Engineering, Turkey, M Gül Department of Geological Engineering, Turkey, E AteΕ Vocational School of AyaΕ, Turkey,
Abstract
Despite threats emanating from the influence of climate and non-climate forcing on the barrier island coastal region of southwestern Nigeria, the extent of the coastal erosion is poorly understood. We report evidence of coastal erosion and sediment accumulation in the region over a 34-year period (1973β2017), using Landsat imagery at intervals of approximately six years. Landsat image corrections and various water-extraction algorithms were used to systematically delineate coastal erosion and accumulation in the area. The region was subdivided into western and eastern subregions separated by Lagos Harbour. In the west, erosion took place during the periods 1973β1979, 1979β1984, 1990β1999 and 2005β2011, whereas in the east, erosion occurred during 1973β1979, 1990β1999 and 1999β2005. Coastal sediment accumulation occurred in the east during 1979β1984, 1984β1990, 2005β2011 and 2011β2017, whereas gains in the west occurred during 1984β1990, 1999β2005 and 2011β2017. The study revealed substantial net erosion of 1 228.1 ha in the region as a whole, over the full period. Sediment accumulation accompanying the coastal erosion appears to be linked to longshore drift. Erosion between 1973 and 2011 was probably attributable to climate change (storms and tidal conditions), longshore drift, the inflow and outflow of water at Lagos Harbour, coastal morphology and, possibly, human impacts. However, the coastal changes between 2011 and 2017 were more obviously associated with human activities, such as development of the Eko Atlantic construction project. Coastal surveillance, together with the use of environmentally sensitive protective measures, could possibly help to reduce coastal erosion in the region. Careful coastal management practices, including artificial nourishing and the installation of resilient structures (e.g. seawalls), should be undertaken to protect human settlements that are already at risk from sea-level rise.
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