
This publication covers a range of disaster risk management (DRM) themes, from community participation in DRM data collection to risk mapping and from urban waste management to hazard accumulation in urban risk traps.
This publication covers a range of disaster risk management (DRM) themes, from community participation in DRM data collection to risk mapping and from urban waste management to hazard accumulation in urban risk traps.
In African cities, orienting risk management towards a developmental agenda can
confront the root causes of poverty and risk. Transition to an integrated approach has
the most chance of success when it combines interventions working on the risk culture
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.
Small- and medium-sized cities and towns in sub-Saharan Africa are growing fast and accumulating risks. Local governments seek to build the resilience of their city in conditions of complex interdependent urban systems and gaps in data and information.
This briefing outlines the development of community-led research to promote urban governance for resilience and how impactful partnerships can be created within a research programme.
Cities are at the centre stage of Africa’s pathway to prosperity, with the majority of its population expected to be living in urban areas within the next decade.
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
Community-based organisation and action can contribute greatly to disaster risk reduction, and interlinked to this, to building resilience to the impacts of climate change.
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.