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192Natural and human-made disastersTable 7.12Disaster incidence andimpacts in Europe(1996–2005)Note: For all disaster types,small events with less than 10mortalities or 100 affectedpeople are not included.Source: EM-DAT, CREDdatabase, University <strong>of</strong>Louvain, Belgium, www.emdat.netNumber <strong>of</strong> events Mortality People affected (thousands) Economic loss (US$million, 2005 value)Avalanches/landslides 18 389 14 20Drought/famines 14 0 1063 8019Earthquakes/tsunamis 52 18,584 4016 29,609Extreme temperatures 79 48,630 771 6706Floods 229 1422 5048 47,860Volcanic eruptions 2 0 0 24Windstorms 110 610 7025 18,138Industrial accidents 56 844 71 11,100Miscellaneous accidents 73 1474 14 874Oceania records <strong>the</strong>lowest incidence <strong>of</strong>disasters for anyregion and hazardtype…EuropeThe role played by relatively high levels <strong>of</strong> economic developmentand political stability in shifting <strong>the</strong> impact <strong>of</strong> disastersfrom human to physical assets can be seen most clearly inthis region (see Table 7.12). This is exemplified by volcaniceruptions, where Europe suffers <strong>the</strong> highest economic losses<strong>of</strong> any region, but no people have been killed or affected.Vulnerability and human loss is highest, compared to o<strong>the</strong>rworld regions, for extreme temperature events. Between1996 and 2005, Europe experienced 47 per cent <strong>of</strong> allextreme temperature events, but 81 per cent <strong>of</strong> all mortalities.Compared with Europe, <strong>the</strong> Americas experienced lessthan half <strong>the</strong> number <strong>of</strong> extreme wea<strong>the</strong>r events, withcomparatively few deaths, but four times <strong>the</strong> numberaffected. This reflects <strong>the</strong> different severity <strong>of</strong> events, butalso greater investment in early warning and response forextreme temperature in <strong>the</strong> Americas.Within Europe, floods were <strong>the</strong> most common disasterbetween 1996 and 2005. Mortality was highest forextreme temperatures, with around 35,000 prematuredeaths from <strong>the</strong> 2003 heat wave alone. 105Europe is a high-income and highly urbanized region.Risk pro<strong>file</strong>s for this region are split between <strong>the</strong> east andwest. Western Europe has strong states and civil societiesproviding good capacity for resilience. It is also a region withrelatively low levels <strong>of</strong> hazard exposure. Eastern Europe ismore variable, with examples <strong>of</strong> strong states but weak civilsociety, and with governance challenges that limit regulation<strong>of</strong> industrial activity and capacity for top-down programmesaimed at vulnerability reduction. This region is also economicallypoorer than Western Europe.OceaniaOceania records <strong>the</strong> lowest incidence <strong>of</strong> disasters for anyregion and hazard type, with <strong>the</strong> exception <strong>of</strong> volcaniceruption (see Table 7.13). This is <strong>the</strong> only region not torecord any industrial accidents from 1996 to 2005. Theregion had <strong>the</strong> lowest economic losses and absolute number<strong>of</strong> people killed and affected by all disaster types. Within <strong>the</strong>region, disasters are most commonly associated withwindstorms, and <strong>the</strong>se result in <strong>the</strong> greatest economiclosses. Earthquakes and tsunamis account for <strong>the</strong> highestlevels <strong>of</strong> mortality.The region is <strong>of</strong> mixed economic status, but with highlevels <strong>of</strong> urbanization. Poorer countries also tend to havegreater political tensions, <strong>of</strong>ten between indigenous andimmigrant populations. Many are small island developingstates facing particular governance challenges within acontext <strong>of</strong> limited human resources. Larger countries,especially New Zealand and Australia, have strong states andcivil societies, as well as robust economies. Yet, inequalityundermines resilience in <strong>the</strong>se multicultural societies. Forlow-lying small island states, sea-level rise due to climatechange will have catastrophic implications.CONCLUDING REMARKSUrban disasters are a product <strong>of</strong> failed urban governance andplanning. Wealth is necessary for building resilience at <strong>the</strong>local and city levels, but is not sufficient in <strong>the</strong> absence <strong>of</strong>governance. Without good governance and open participationin urban planning, economic development too <strong>of</strong>tenleads to inequality and failures to implement regulation in<strong>the</strong> industrial and residential sectors.The relationships between urbanization and disasterrisk are dynamic. Past urban civilizations have collapsedTable 7.13Disaster incidence andimpacts in Oceania(1996–2005)Note: For all disaster types,small events with less than 10mortalities or 100 affectedpeople are not included.Source: EM-DAT, CREDdatabase, University <strong>of</strong>Louvain, Belgium, www.emdat.netNumber <strong>of</strong> events Mortality People affected (thousands) Economic loss (US$million, 2005 value)Avalanches/landslides 8 128 1 No dataDrought/famines 8 88 1083 329Earthquakes/tsunamis 9 2201 36 No dataExtreme temperatures 1 0 0 221Floods 38 34 96 1735Volcanic eruptions 7 4 49 No dataWindstorms 72 255 832 2859Industrial accidents 0 0 0 No dataMiscellaneous accidents 4 46 12 No data

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