Managing Coastal Risks in West Africa

Coastal erosion is a naturally occurring process that is accelerated by human impacts. Artificial stabilization of the shoreline, the deterioration of natural formations, the construction of infrastructure, the extraction of materials, and the proliferation of dams deprive fragile coastal areas of important sediment deposits, which leads to erosion. Degradation of the shoreline reduces the natural protection of coastal areas to storm surges, which, together with heavy precipitation, exposes low-lying areas to flooding. Given the trans boundary nature of the region’s ecosystems, the potential downstream effects of infrastructure, and the importance of the coastline for all sectors, optimal solutions to reduce the risk along West Africa’s coasts can be reached only through multi sectoral action and multinational cooperation. Every national and regional development plan in West Africa should take coastal risks and adaption to climate change into consideration.

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Bibliographic Details
Main Author: World Bank Group
Format: Brief biblioteca
Language:English
en_US
Published: World Bank, Washington, DC 2015-01
Subjects:FLOODING, RISKS, WASTE WATER, ECOSYSTEM, STORM, EARLY WARNING, DISASTER RISK, CLIMATE CHANGE, HIGH TIDES, BEACHES, RISK REDUCTION, NATURE, WATER DRAINAGE, AQUACULTURE, LAND USE PLANNING, BANK, STORMS, RAPID POPULATION GROWTH, CONTINGENCY PLANS, FORESTS, PROTECTION, STABILIZATION, AGRICULTURAL LANDS, DAMAGE, SHORELINES, COASTAL AREAS MANAGEMENT, DISASTER, COASTAL ZONE, ISLANDS, WATER RESOURCES, EROSION, COASTS, SEDIMENT, LAND, ECOSYSTEMS, COASTLINE, MANGROVE, COAST, RISK, ESTUARIES, LEADS, POPULATION GROWTH, SHORELINE, STORM SURGES, DISASTER RISK REDUCTION, CONSTRUCTION, WATER, COASTAL EROSION, COASTAL ENVIRONMENTS, SEA-LEVEL, LIVELIHOODS, SEA, DISASTERS, TIDES, COASTLINES, STORM WATER, SEA LEVEL, SWAMPS, MANGROVE FORESTS, COASTAL AREAS, FISHING, LAGOONS, LAND USE,
Online Access:http://documents.worldbank.org/curated/en/2015/11/25486902/managing-coastal-risks-west-africa
http://hdl.handle.net/10986/24281
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