The WorldRiskIndex 2016: Reveals the Necessity for Regional Cooperation in Vulnerability Reduction

Author:

Birkmann Joern1,Welle Torsten1

Affiliation:

1. University of Stuttgart, Institute of Spatial and Regional Planning, Germany

Abstract

Extreme events do not necessarily trigger extreme impacts. Exposure and vulnerability levels often decide whether hazards and extreme events lead to disasters or severe suffering or not. Measuring and assessing different levels of exposure, vulnerability and risk is therefore crucial in order to inform decision making and to provide guidance for defining priorities for risk reduction and adaptation. The WorldRiskIndex (WRI) is an approach to assess global exposure, vulnerability and risk patterns based on national scale resolution data. The new results of the WRI 2016 underscore that risk of natural hazards and climate change is particularly high in Oceania, Southeast Asia, Sub-Saharan Africa and the Caribbean as well as Central America. The assessment for 171 countries reveals important improvements in some countries, such as Namibia, however, in other countries such as Brunei, Darussalam and Serbia risk has increased, particularly due to higher susceptibility and lower coping and adaptive capacities to deal with extreme events and natural hazards. The analysis of global patterns of risk shows that not only the physical exposure to extreme events or natural phenomena but also the societal context conditions in countries like Vanuatu, Niger, Haiti and Afghanistan are key drivers of risk and therefore efforts for risk reduction and adaptation at the local and national level need to also address aspects such as poverty and corruption. The persistence of high risk in various countries in Africa and Oceania also suggests that it is likely that these countries might not be able to effectively reduce risks solely on their own but rather need regional approaches and institutions for risk reduction and adaptation.

Publisher

World Scientific Pub Co Pte Lt

Subject

General Medicine

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