There have been formal commitments by national governments to empower Local Governments (LGs) to undertake practical DRR actions as part of the Sendai Framework for Disaster Risk (SFDDR) (2015-2030) and UNISDR’s Making Cities Resilient Campaign.
Urbanization is a major feature of global population redistribution, and Sub-Saharan Africa (SSA), though currently ranked as the least urbanized region of the world, is the most rapidly urbanizing globally.
Between 2016 and 2017, Arup carried out case study research to explore how large two infrastructure projects are creating, compounding or mitigating risk in Nairobi. The Thika Highway Improvement Project and the Two Rivers Mall Development were selected as case studies as they represent typical l
Cette recherche contribue à la littérature sur le risque de catastrophes, en approfondissant la compréhension de la relation entre la vulnérabilité aux inondations, l'urbanisme et les stratégies d'adaptation locales.
Capitale du Niger depuis 1926, la communauté urbaine de Niamey couvre une superficie de 255 km². Elle dispose de cinq communes dont quatre (I, II, III, IV) se trouvent sur la rive gauche et la commune V à la rive droite.
The lack of systematic and homogenous records of people being impacted by everyday hazards and disaster events at all scales in many African cities is a major limitation to effective planning for risk reduction.
In recent years, lives and property worth millions of dollars have been destroyed in fire disasters in secondary schools around the world. Cases of fire disasters in Nigerian secondary schools have been experienced in the last decade with increasing frequency and severity.
Urban flooding cannot be avoided entirely and in all areas, particularly in coastal cities. Therefore adaptation to the growing risk is necessary. Geographical Information Systems (GIS) based knowledge on risk informs location-based approach to adaptation to climate risk.
Nairobi has a subtropical highlands climate. It is located close to the eastern edge of the East African Rift Valley at an altitude of roughly 1800 metres above sea level which strongly influences its climate.
This document provides a summary of the historic climate at Karonga and how it is projected to change into the future due to anthropogenic climate change.