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SCENARIOS OF GIANT TSUNAMIS OF TECTONIC ORIGIN IN THE MEDITERRANEAN

机译:地中海构造构造的巨大海啸

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Scenarios represent a very useful technique for the definition and evaluation of tsunami hazard and risk for any given region, and a basic step in the frame of tsunami mitigation and preparedness and of sustainable coastal zone development. With the exception of very few countries, like Japan and the United States, emergency plans in the rest of the world have never taken serious care of tsunamis until the occurrence of the giant Indian Ocean tsunami on December 26, 2004. That event dramatically brought the problem of tsunami hazard and risk assessment to the general attention and showed the urgent need for implementation of t&unami early warning systems (TEWSs). The problem is particularly urgent for the Mediterranean countries that are known to have been attacked by numerous tsunamis in the past, several of which had catastrophic size and impact. This paper is an attempt to develop some simple scenarios of earthquake-generated tsunamis in the Mediterranean. We identify four different seismogenic areas in the western, central and eastern sectors of the basin. For each of them, we take into account a seismic fault capable of generating an earthquake with magnitude equal or larger than the highest magnitude registered in that region in historical times. Then we simulate numerically the ensuing tsunamis, highlighting the basic features of the wave propagation and roughly identifying the coastal sectors that are expected to suffer the heaviest tsunami effects. One of the most important outcomes is that these scenario tsunamis attack the nearest coasts within at most 15 minutes, which poses serious constraints for designing appropriate TEWS for the Mediterranean.
机译:方案是定义和评估任何给定区域的海啸危害和风险的非常有用的技术,是减轻海啸和备灾以及沿海地区可持续发展框架的基本步骤。除极少数国家(如日本和美国)外,直到2004年12月26日发生印度洋海啸之后,世界其他地区的应急预案才从未认真对待过海啸。海啸危害和风险评估问题引起了普遍关注,并表明迫切需要实施海啸预警系统。对于过去已知遭受过无数海啸袭击的地中海国家来说,这个问题尤为紧迫,其中一些海啸造成了灾难性的规模和影响。本文是尝试开发一些简单的地中海地震引发海啸的方案。我们在盆地的西部,中部和东部地区确定了四个不同的地震发生区。对于它们中的每一个,我们都考虑到一个地震断层,该断层能够产生震级等于或大于该历史时期该地区记录的最高震级的地震。然后,我们对随后发生的海啸进行数值模拟,突出显示了海浪传播的基本特征,并大致确定了预计将遭受最严重海啸影响的沿海地区。最重要的结果之一是,这些海啸情景最多在15分钟内袭击了最近的海岸,这给设计适合地中海的TEWS构成了严重的限制。

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