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A deterministic analysis of tsunami hazard and risk for the southwest coast of Sri Lanka

机译:斯里兰卡西南海岸海啸危险性和风险的确定性分析

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This paper describes a multi-scenario, deterministic analysis carried out as a pilot study to evaluate the tsunami hazard and risk distribution in the southwest coast of Sri Lanka. The hazard and risk assessment procedure adopted was also assessed against available field records of the impact of the Indian Ocean tsunami in 2004. An evaluation of numerically simulated nearshore tsunami amplitudes corresponding to 'maximum-credible' scenarios from different subduction segments in the Indian Ocean surrounding Sri Lanka suggests that a seismic event similar to that generated the tsunami in 2004 can still be considered as the 'worst-case' scenario for the southwest coast. Furthermore, it appears that formation of edge waves trapped by the primary waves diffracting around the southwest significantly influences the nearshore tsunami wave field and is largely responsible for relatively higher tsunami amplitudes in certain stretches of the coastline under study. The extent of inundation from numerical simulations corresponding to the worst-case scenario shows good overall agreement with the points of maximum penetration of inundation from field measurements in the aftermath of the 2004 tsunami. It can also be seen that the inundation distribution is strongly influenced by onshore topography. The present study indicates that the mean depth of inundation could be utilised as a primary parameter to quantify the spatial distribution of the tsunami hazard. The spatial distribution of the risk of the tsunami hazard to the population and residential buildings computed by employing the standard risk formula shows satisfactory correlation with published statistics of the affected population and the damage to residential property during the tsunami in 2004.
机译:本文描述了一项多情景,确定性分析,作为一项初步研究来评估斯里兰卡西南海岸的海啸危害和风险分布。还根据2004年印度洋海啸影响的现有现场记录对所采用的危害和风险评估程序进行了评估。对印度洋周边不同俯冲段的“最大可信”情景对应的数值模拟近岸海啸振幅进行了评估斯里兰卡认为,与2004年海啸类似的地震事件仍可被视为西南海岸的“最坏情况”。此外,似乎是由在西南方向绕射的初级波所捕获的边波的形成显着影响了近海海啸波场,并且在所研究的海岸线的某些范围内,是造成海啸振幅相对较高的主要原因。来自与最坏情况对应的数值模拟的淹没程度显示出与2004年海啸后实地测量的淹没最大穿透点完全一致。还可以看出,淹没分布受到陆上地形的强烈影响。本研究表明,平均淹没深度可以用作量化海啸危害空间分布的主要参数。通过使用标准风险公式计算的海啸危害人口和住宅建筑物风险的空间分布与2004年海啸期间受影响人口和住宅财产的破坏统计数据显示出令人满意的相关性。

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