Compound Coastal Flooding and Climate Change in the Niger Delta:Hydro-Climatic Modelling And Engineering Adaptation A Synthesis and Conceptual Modelling Framework
Authors
Centre for Disaster Risk Management and Development Studies, University of Port Harcourt, Nigeria (Nigeria)
Department of Environmental Management, Rivers State University, Port Harcourt, Nigeria (Nigeria)
Department of Environmental Management, Rivers State University, Port Harcourt, Nigeria (Nigeria)
Department of Environmental Management, Rivers State University, Port Harcourt, Nigeria (Nigeria)
Centre for Disaster Risk Management and Development Studies, University of Port Harcourt, Nigeria (Nigeria)
Article Information
DOI: 10.47772/IJRISS.2026.100900388
Subject Category: Compound Flooding
Volume/Issue: 10/9 | Page No: 5772-5785
Publication Timeline
Submitted: 2026-09-20
Accepted: 2026-09-24
Published: 2026-10-12
Abstract
The Niger Delta, Africa's largest deltaic and mangrove ecosystem, is increasingly exposed to compound coastal flooding the co-occurrence or successive interaction of fluvial discharge, pluvial runoff, storm surge, tidal elevation, and relative sea-level rise (RSLR) driven by anthropogenic climate change, land subsidence from hydrocarbon extraction, and rapid, unplanned coastal urbanisation. This paper synthesises the peer-reviewed and grey literature on compound flooding processes, hydro-climatic modelling frameworks, and engineering and nature-based adaptation options, and applies that synthesis to the Niger Delta as a regional case study. Evidence reviewed indicates that the Gulf of Guinea coastline is experiencing sea-level rise at approximately 3.9 mm/yr roughly 10% above the global average while localised land subsidence associated with hydrocarbon withdrawal (25–125 mm/yr at active well fields) compounds this signal into a relative sea-level rise of up to ~0.96 m by 2050 in the most affected settlements. Concurrently, regional rainfall intensity increased by an estimated 53% between 2012 and 2017 and a further 12% between 2017 and 2022, while upstream dam operations on the Niger and Benue river systems modulate the timing and magnitude of downstream discharge peaks. A conceptual hydro-climatic modelling framework coupling rainfall–runoff, river-routing, and storm-surge/tide hydrodynamic components is proposed for the region, drawing on established compound-inundation modelling practice (e.g., HEC-RAS, MIKE 21, ADCIRC-class coupling). Engineering adaptation options are evaluated along a grey–green–hybrid continuum, with particular attention to mangrove-fronted dike systems, elevated infrastructure, and adaptive, sensor-linked flood defences. The paper concludes that reducing compound flood risk in the Niger Delta requires integrated, basin-to-coast hydro-climatic modelling; regulation of subsidence-inducing extraction; mangrove restoration at scale; and hybrid engineering investment prioritised in the most exposed core states of Bayelsa, Rivers, and Delta.
Keywords
compound flooding; Niger Delta; sea-level rise; land subsidence; hydro-climatic modelling; coastal engineering; nature-based adaptation; climate change.
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