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Quantitative Tsunami Risk Assessment in Terms of Building Replacement Cost Based on Tsunami Modelling and GIS Methods: The Case of Crete Isl., Hellenic Arc

机译:基于海啸建模和GIS方法的建筑物替代成本方面的定量海啸风险评估:克里特岛的案例。,希腊电弧

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Tsunami risk assessment is an important component of the planning for risk reduction. We considered tsunami risk as a convolution of tsunami hazard, vulnerability of the assets at risk (e.g. buildings) and the economic value exposed. For testing the model, a coastal segment at the west of Heraklion, capital city of Crete Isl., Greece, was selected. Heraklion was hit in the past by strong tectonic and volcanic tsunamis, generated along the Hellenic Arc in the Mediterranean region. The Minoan tsunami produced by pyroclastic flows during the LBA (17th century BC) great eruption of Thera (Santorini) was selected as an extreme tsunami scenario for the hazard (inundation) zone determination through numerical simulation based on Boussinesq equations for fully non-linear waves. It was found that the wave penetrates inland up to1.2km, while the maximum water depth is14m. The building stock was obtained from the 2011 national census data and validated with the use of orthophotomaps, field inspection and Google Maps. Building vulnerability was determined with the use of the empirical GIS tool DAMASCHE which is based on 2004 Indian Ocean tsunami building damage data and produces damage level by combining water depth and building construction types. The damage level was translated to absolute monetary loss on the basis of cost flat rates determined officially for building replacement, i.e., either reparation or reconstruction, after the destructive earthquakes in Greece during 2014. The method is applicable in other parts of the Mediterranean and beyond provided that appropriate data are available.
机译:海啸风险评估是减少风险规划的重要组成部分。我们将海啸风险视为海啸危害的卷积,危险的资产脆弱性(例如建筑物)和暴露的经济​​价值。为了测试模型,选择了克里特岛首都克里特岛的沿海地区沿海地区。,希腊,希腊。伊拉克利翁在过去的强大的构造和火山海啸中被击中了过去,沿着地中海地区的希腊弧线产生。通过基于BoussinesQ方程的危害(淹没)区的极端海啸场景,通过基于BoussinesQ方程的危险(淹没)区测定的危险(Santorini)在LBA(Santorini)爆发的Minoan海啸中被选为危险(Santorini)的爆发。 。发现波浪渗透到内陆,最大水深为14米。建筑物股票从2011年国家人口普查数据获得,并验证了使用正轨,现场检查和谷歌地图。通过使用基于2004印度洋海啸建设损伤数据的经验GIS工具DAMASCHE确定了建筑漏洞,并通过组合水深和建筑施工类型来产生损坏水平。在2014年希腊的破坏性地震后正式确定的成本统一率,损害级别被转化为绝对货币损失。该方法适用于地中海及其他地区的方法适用于其他地区只要适当的数据可用。

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