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Tsunamigenic potential of crustal faults and subduction zones in the Mediterranean

机译:地中海地壳断层和俯冲带的海啸潜在

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摘要

We compiled a database and systematically evaluated tsunamigenic potential of all up-to-date known crustal fault systems and subduction zones in the entire Mediterranean region that has experienced several catastrophic tsunamis in historical times. The task is accomplished by means of numerical modeling of tsunami generation and propagation. We have systematically simulated all representative ruptures populating known crustal faults and subduction interfaces with magnitudes ranging from 6.1 up to expected Mwmax. Maximum tsunami heights calculated everywhere along the coasts allowed us to classify the sources in terms of their tsunamigenic potential and to estimate their minimum tsunamigenic magnitude. Almost every source in the Mediterranean, starting from Mw = 6.5, is capable to produce local tsunami at the advisory level (wave height >20 cm and ≤50 cm). In respect to the watch level (wave height >50 cm) larger magnitudes are needed (Mw ≥ 6.9). Faults behave more heterogeneously in the context of far field early warning. De-aggregation of the database at any selected coastal location can reveal relevant sources of tsunami hazard for this location. Our compilation blueprints methodology that, if completed with source recurrence rates and site-specific amplification factors, can be considered as a backbone for development of optimal early warning strategies by Mediterranean tsunami warning providers.
机译:我们收集了一个数据库,并系统地评估了整个地中海地区所有历史上经历过几次灾难性海啸的最新已知地壳断层系统和俯冲带的海啸成因潜力。该任务是通过海啸发生和传播的数值模型来完成的。我们已经系统地模拟了所有已知的破裂,这些破裂充满了已知的地壳断层和俯冲界面,震级范围从6.1到预期的Mwmax。沿海岸到处计算的最大海啸高度使我们能够根据海啸的潜在成因对来源进行分类,并估算其最小海啸的大小。从Mw = 6.5开始,地中海地区几乎所有来源都能够在建议水平(波高> 20 cm和≤50cm)产生局部海啸。对于表高度(波高> 50 cm),需要更大的幅度(Mw≥6.9)。在远场预警的背景下,断层表现得更加异质。在任何选定的沿海位置对数据库进行分解汇总,可以揭示该位置的海啸危害的相关来源。我们的编制蓝图方法论,如果加上源复发率和特定地点的扩增因子,可以被视为地中海海啸预警提供者制定最佳预警策略的基础。

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