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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Historical tsunamis and present tsunami hazard in eastern Indonesia and the southern Philippines
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Historical tsunamis and present tsunami hazard in eastern Indonesia and the southern Philippines

机译:印度尼西亚东部和菲律宾南部的历史海啸和当前海啸危害

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摘要

Eastern Indonesia and the southern Philippines comprise a huge and seismically highly active region that has received less than the deserved attention in tsunami research compared with the surrounding areas exposed to the major subduction zones. In an effort to redress the balance the tsunami hazard in this region is studied by establishing a tsunami event database which, in combination with seismological and tectonic information from the region, has allowed us to define and justify a number of 'credible worst-case' tsunami scenarios. These scenarios have been used in numerical simulations of tsunami generation and propagation to study maximum water level along potentially affected shorelines. The scenarios have in turn been combined to provide regional tsunami hazard maps. In many cases the simulations indicate that the maximum water level may exceed 10 m locally and even reach above 20 m in the vicinity of the source, which is of the same order as what is forecasted along the Sumatra and Java trenches for comparable return periods. For sections of coastlines close to a source, a tsunami may strike only a few minutes after it is generated, providing little time for warning. Moreover, several of the affected areas are highly populated and are therefore also high risk areas. The combination of high maximum water levels, short warning times, dense populations, and relatively short return periods suggests strongly that the tsunami hazard and risk in these regions are alarmingly high.
机译:印度尼西亚东部和菲律宾南部是一个巨大且地震活跃的地区,与暴露于主要俯冲带的周边地区相比,在海啸研究中受到的关注不足。为了纠正这种平衡,通过建立海啸事件数据库来研究该地区的海啸危害,该数据库与该地区的地震学和构造信息相结合,使我们能够定义和证明一些“可信的最坏情况”海啸场景。这些方案已用于海啸产生和传播的数值模拟中,以研究沿可能受影响的海岸线的最大水位。这些情景又被组合起来,以提供区域海啸灾害图。在许多情况下,模拟表明,最大水位可能在当地超过10 m,甚至在水源附近达到20 m以上,这与沿苏门答腊和爪哇海沟在可比的回水期预测的水位相同。对于靠近源头的海岸线部分,海啸可能仅在几分钟后发生,因此预警时间很少。此外,一些受影响的地区人口稠密,因此也是高风险地区。最大最高水位高,警告时间短,人口稠密以及返回时间相对较短的组合强烈表明,这些地区的海啸危险和风险令人震惊地高。

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