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Map of integrated risk for Portugal counties 

Map of integrated risk for Portugal counties 

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At the forefront of the Global Earthquake Model (GEM) is the development of uniform standards, datasets, and state-of-the-art modeling tools for the communication of earthquake risk. For a more holistic assessment of the scale and consequences of earthquake impacts, spatially enabled and open databases, methods, and Open Source software tools are b...

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... Each sub-component was then summed to derive a final composite score. Since there are five sub-components, the summed score of the composite index ranges between 0 and 5 (0 being the least socially vulnerable and 5 being the most). As a subsequent step, the composite social vulnerability scores were rescaled using Min-Max rescaling to produce a final composite score between zero and one (0 being the least socially vulnerable and 1 being the most vulnerable). An aggregation method using equal weights was applied due to the lack of theoretical justification for weighting one variable over another for use in this proof of concept. The evaluation of integrated risk (i.e. the combination of estimated losses with the social vulnerability index outlined above) required the modeling of expected economic losses for each county (or first order impacts) and the modeling of conditions within social systems that create the potential for harm and loss. The modeled losses in the form of estimates of average annual loss for each county were also rescaled using the Min-Max rescaling method to render them commensurate to the social vulnerability index. To derive an estimate of integrated risk, a total risk index was constructed via the convolution of the social vulnerability index with the estimates of physical earthquake risk. Carreño et al. (2007; 2012) provide the aggregation method that was adopted for this work due to its mathematical simplicity. In this method, the direct potential impact of an earthquake (in a general sense) is denoted as R T = R F ( 1 + F ) where R T is a total risk index, R F is a physical earthquake risk index which is an average annual loss estimate for Portugal derived utilizing the physical risk model outlined above, and F is the composite social vulnerability index which may be described as an aggrevating coefficient of the estimated loss. The probabilistic seismic hazard for mainland Portugal was calculated using the Classical PSHA- based hazard calculator (Pagani et al. 2014). A large number of seismic hazard curves were derived following a 0.01x0.01 decimal degrees spatial resolution considering a wide spectrum of epistemic uncertainties (e.g. various ground motion prediction models, seismic zonations, magnitude-frequency distributions), through the employment of a logic tree structure. Using the set of hazard curves at each location, a mean seismic hazard map for a probability of exceedance of 10% in 50 years was calculated, as depicted in Figure 2. The appraisal of the spatial distribution of hazard in Portugal indicates an expected higher peak ground acceleration on rock for the Lower Tagus Valley (region around Lisbon) and the south of Portugal, thus highlighting regions where a combination of seismically vulnerable structures and high population concentration could lead to significant earthquake losses. The hazard results were combined with the exposure and vulnerability models to derive loss exceedance curves for each county. These curves were converted into annual rate of exceedance, and numerically integrated in order to obtain the average annual economic loss, as illustrated in Figure 3. In addition to hazard and physical risk, understanding the distribution of the social vulnerability of populations is an integral part of disaster management, planning, and mitigation. Figure 4 depicts the spatial variation in social vulnerability for Portugal’s counties. The classification scheme was simplified (i.e. high, moderate, low) for presentation purposes. The counties delineated in the darker shades of red along the classification continuum exhibit higher levels of social vulnerability. While the spatial pattern is not uniform throughout, there are significant pockets of social vulnerability that could warrant management concern given the seismic threat. Of special interest is the clustering of moderate to high and high levels of social vulnerability in the southwestern portion of the country. Here, counties that host cities such as Santarem, Setubal, and Faro have populations with high levels of social vulnerability. These areas are also in zones of high seismicity (see Figure 2) and zones of high physical earthquake risk (see Figure 3). In addition to these clusters of counties with high social vulnerability and physical risk, there is another large section in Portugal’s northern portion with high levels of social vulnerability. These are in largely rural areas outside of the high-risk zones. However, exceptions in these areas exist where counties are exposed to considerable risk of loss and that also contain highly socially vulnerable populations. Populations within these counties may not only suffer greater impacts due to ground shaking and building damage, they may also lack the ability to adequately mitigate, prepare for, and recover from a damaging earthquake event. The spatial distribution of risk within these counties is compounded when viewed as an integrated risk map (Figure 5). The impacts from an earthquake will be expressed differentially across communities. To be effective, governments, disaster planners, and managers must not only understand the physical agents of earthquake risk, but also the social characteristics that give rise to vulnerabilities within the communities they protect. This paper presented a method, workflow, and analysis conducted within GEM’s OpenQuake that consists of a spatial delineation of physical earthquake risk combined with an index of social vulnerability. The overall approach leads to an encompassing perspective on risk assessment that considers loss and damage as part of a dynamic system, and our findings suggest that there are spatial differences in physical earthquake risk, social vulnerability, and integrated risk within Portugal. Disaster mitigation and planning under such circumstances may require special attention where different aspects of social vulnerability affect the way in which communities may prepare for and respond to the seismic threat. In sum, the approach mainstreams risk and social vulnerability into policy discussions on earthquake loss and damage reduction, makes it possible to use risk estimates in benchmarking exercises to monitor changes in loss potential over time, and recognizes that both the causes and solutions for earthquake loss are found in human, environmental, and built-environment relationships. Boruff BJ and Cutter SL (2007) “The Environmental Vulnerability of Caribbean Island Nations,” Geographical Review, 97(1): 932-942 Burton, CG and Cutter SL (2008) “Levee Failures and Social Vulnerability in the Sacramento-San Joaquin Delta Area, California, “ Natural Hazards Review” , 9(3): 136-149 Burton CG, Khazai B, Silva V, (in press) “Social Vulnerability and Integrated Risk Assessment within the Global Earthquake Model”, Proceedings of 10 th National Conference in Earthquake Engineering , Earthquake Engineering Research Institute, Anchorage, Alaska Cardona, OD (2005) Indicators of Disaster Risk and Risk Management, IADB-UNC/IDEA Program for Latin America and the Caribbean, Universidad Nacional de Colombia, Instituto de Estudios Ambientales (IDEA), Manizales Carreño M-L, Cardona OD, Barbat AH (2007) “Urban Seismic Risk Evaluation: A Holistic Approach,” Natural Hazards, 40: 137-172 Carreño M-L, Cardona OD, Barbat AH (2012) “New Methodology for Urban Seismic Risk Assessment from a Holistic Perspective,” Bulletin of Earthquake Engineering , 40: 137-172 Carvalho EC, Coelho E, Campos Costa A, Sousa ML, Candeias P (2002) “Vulnerability Evaluation of Residential Buildings in Portugal,” Proceedings of the 12th European Conference on Earthquake Engineering , London, United Kingdom Cutter, SL (1996) “Vulnerability to Environmental Hazards,” Progress in Human Geography , 20: 529-539 Cutter SL, Boruff BJ, Shirley WL (2003) “Social Vulnerability to Environmental Hazards,” Social Science Quarterly , 84: 242-261 Cutter SL, Mitchell J, Scott M (2000) “Revealing the Vulnerability of People and Places: A Case Study of Georgetown County, South Carolina,” Annals of the Association of American Geographers, 90 (4): 713-737 Davidson, R (1997) “A Multidisciplinary Urban Earthquake Disaster Risk Index,” Earthquake Spectra , 13(2): 211-223 Fekete, A (2009) “Validation of a Social Vulnerability Index in Context to River-floods in Germany,” Natural Hazards and Earth Systems Sciences , 9: 393-403 Fernandez J, Mattingly S, Bendimerad F, Cardona OD (2006) Application of Indicators in Urban and Megacities Disaster Risk Management, A Case Study of Metro Manila, EMI Topical Report TR-07-01 Freudenberg M (2008) Composite Indicators of Country Performance: A Critical Assessment , OECD, Paris Hewitt K and Burton I (1971) The Hazardousness of a Place: A Regional Ecology of Damaging Events, University of Toronto Press, Toronto Khazai B and Bendimerad F. (2011) Risk and Resiliency Indicators, EMI Topical Report TR-1 1-03 Khazai B, Kilic O, Basmaci A, Konukcu B, Sungay B, Zeidan A, Wenzel F (2008) Megacity Indicators System for Disaster Risk Management - Implementation in Istanbul, in M ...

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Capacity development at all levels of society, comprehensive knowledge management and the involvement of science in public awareness-raising, media communication, behaviour change, and education campaigns should be strengthened. Specific tools should be developed to facilitate science, technology and innovation outputs to help inform policy-making and practice. Additionally institutions and individuals at risk of disasters should be invited to participate in scientific research (surveys, vulnerability assessments and other activities ) to collect local knowledge and create reliable databases should be created and so that information can be used to tailor initiatives to the local context while enabling global comparisons and assessments. 2. Use a multidisciplinary approach to research An all-hazard, risk-based, problem-solving, results-oriented approach should be used in DRR research to address the multifactorial and interdependent nature of the disaster risk chain and to identify relevant solutions and optimize the use of resources. Synergies with the climate change and sustainable development agenda should continue to be articulated and leveraged. This requires collaboration and communication across the scientific disciplines and technical fields, and with all stakeholders including representatives of governmental institutions, communities of policy making, scientific and technical specialists, the technology sector and members of the communities at risk to guide scientific research, set research agendas and support scientific education and training. The potential contribution of affected and vulnerable communities in generating research questions, and in performing research collaboratively or independently, should be valued and facilitated. 3. Build systems resilience through local, national, regional and international partnerships Science and technology communities wish to strengthen the dialogue and collaboration with policy-makers and DRR practitioners at local, national, regional and global levels to identify needs and knowledge gaps, co-design, co-produce and co-deliver new knowledge, and make science more readily available and accessible. To this end, science and technology communities and networks will mobilise and strengthen existing capacities and initiatives, including national platforms/bodies, to support the implementation of the post-2015 framework for DRR from the local to the global scale, and in particular deliver outputs.
Chapter
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