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Modelling of Earthquake-Induced Tsunami in the Eastern Mediterranean Region

机译:地中海东部地震诱导的海啸建模

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A number of tsunamigenic zones in the Eastern Mediterranean region were investigated. Historically, the strongest tsunami waves are excited in the Hellenic and Cyprus arcs, the Aegean Sea and the Levantine coast. We modelled the generation of tsunami specifying the epicenter, the focal mechanism, and the maximum of the observed magnitude for each considered tsunamigenic zone. Our approach is based on the numerical simulations of tsunami waves, performed by the code UBO-TSUFD, developed in the University of Bologna. Initial displacement of the sea floor is calculated in accordance with Okada's formulas. We focused our discussion on the tsunami impact on the coasts of Karpathos, Cyprus and Levantine countries. Tsunami parameters are computed for each scenario and results are used to build maps of the computed maximum tsunami heights. Synthetic mareograms are simulated for several points near some important coastal cities of the study area.
机译:调查了东地中海东部地区的许多海啸区。从历史上看,最强大的海啸波浪在希腊和塞浦路斯弧线,爱琴海和莱尼琳海岸兴奋。我们建模了关于震所,焦平机构的海啸,焦点机制,以及每个考虑的海啸区的最大值的产生。我们的方法是基于由博洛尼亚大学开发的代码UBO-TSUFD执行的海啸波的数值模拟。海底的初始位移是根据冈田的公式计算的。我们专注于我们对海啸对塞浦路斯,塞浦路斯和莱曼丁国家的海岸的影响。对于每个场景计算海啸参数,结果用于构建计算的最大海啸高度的映射。在研究区的一些重要沿海城市附近的几个要点模拟了合成的Mareoxps。

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