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An Analysis of Fatality Ratios and the Factors That Affected Human Fatalities in the 2011 Great East Japan Tsunami

机译:2011年东日本海啸的死亡率和影响人类死亡的因素分析。

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This study presents a new analysis of spatial variation in fatality ratios in the 2011 Great East Japan tsunami, in order to overcome the limitations of previous studies that tended to underestimate the fatality ratios. In addition, this analysis was performed in a manner that allows the results to be compared to those from analyses of fatality ratios in other historical tsunamis. To do this, it uses population and fatality data at the village scale in areas of less than 3 km2 where the inundation ratio was greater than 70%, rather than the lower-resolution data used in previous studies. The median value of the tsunami inundation depth at each location was extracted at the original 5-m grid resolution. All of the data were obtained from the Reconstruction Support Survey Archive. Based on the results, a strong correlation between the fatality ratio and inundation depth was found only in some areas of the Sendai Plain, whereas no strong correlation was observed along the Sanriku ria coastline. Fatality ratios in Sanriku were likely related not only to the force of the tsunami but also to other factors, such as the ria topography and the populationa??s experience of past historical tsunamis. Data from other tsunamis in regions where tsunamis frequently occur also indicate that historical tsunami experience is a key factor in reducing fatality ratios. In contrast, the Sendai Plain shows smaller variation in local tsunami amplification effect compared to that of the Sanriku ria coastline, as well as fewer coastal defence structures. Therefore, the fatality ratio in that region was predominantly affected by the force of the tsunami and the residentsa?? individual characteristics. On the Sendai Plain, Ishinomaki City exhibited a strong correlation between the fatality ratio and inundation depth, as well as between fatality ratio and building damage because its low evacuation ratio meant that many fatalities occurred in victimsa?? homes. Therefore, the fatality ratio in Ishinomaki City was higher than those in other areas at the same inundation depth. Simple empirical formulas were developed for estimation of human fatalities based on inundation depths and building damage ratios.
机译:这项研究提出了一种新的分析方法,用于分析2011年东日本大地震海啸中的死亡率的空间变化,以克服以前的研究的局限性,这些研究往往低估了死亡率。另外,以允许将结果与来自其他历史海啸中的死亡率的分析结果进行比较的方式执行该分析。为此,它使用淹没率大于70%的小于3 km2的村庄规模的人口和死亡数据,而不是先前研究中使用的较低分辨率的数据。以原始的5米网格分辨率提取每个位置的海啸淹没深度的中值。所有数据均来自“重建支持调查档案”。根据结果​​,仅在仙台平原的某些地区发现了死亡率和淹没深度之间的强相关性,而在三陆河沿岸地区则没有发现强相关性。 Sanriku的死亡率很可能不仅与海啸的影响有关,而且还与其他因素有关,例如ria的地形和过去历史海啸的人口数量。来自海啸频繁发生地区的其他海啸的数据也表明,历史的海啸经历是降低死亡率的关键因素。相比之下,仙台平原与三陆河沿岸地区相比,局部海啸放大效应的变化较小,海防结构也较少。因此,该地区的死亡率主要受海啸和居民的影响。个人特征。在仙台平原上,石卷市的死亡率与淹没深度,死亡率与建筑物破坏之间都具有很强的相关性,因为其疏散率低意味着受害人中有很多死亡。家园。因此,在淹没深度相同的情况下,石卷市的死亡率高于其他地区。开发了简单的经验公式,用于根据淹没深度和建筑物破坏率估算人员死亡人数。

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