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Scenarios of Earthquake-Generated Tsunamis for the Italian Coast of the Adriatic Sea

机译:意大利亚得里亚海沿岸发生地震海啸的情景

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We calculated the expected impact on the Italian coast of the Adriatic Sea of a large set of tsunamis resulting from potential earthquakes generated by major fault zones. Our approach merges updated knowledge on the regional tectonics and scenario-like calculations of expected tsunami impact. We selected six elongated potential source zones. For each of them we determined a Maximum Credible Earthquake and the associated Typical Fault, described by its size, geometry and kinematics. We then let the Typical Fault float along strike of its parent source zone and simulated all tsunamis it could generate. Simulations are based on the solution of the nonlinear shallow water equations through a finite-difference technique. For each run we calculated the wavefields at specified simulation times and the maximum water height field (above mean sea level), then generated travel-time maps and maximum water height profiles along the target coastline. Maxima were also classified in a three-level code of expected tsunami threat.
机译:我们计算了由主要断层带产生的潜在地震造成的大量海啸对亚得里亚海意大利海岸的预期影响。我们的方法将有关区域构造的最新知识与预期海啸影响的类似情景的计算相结合。我们选择了六个拉长的潜在源区。对于每个地震,我们确定了最大可信地震和相关的典型断层,由其大小,几何形状和运动学描述。然后,我们让典型断层沿着其父源区的走向浮动,并模拟它可能产生的所有海啸。模拟是通过有限差分技术基于非线性浅水方程的求解。对于每次运行,我们都计算了指定模拟时间的波场和最大水高场(平均海平面以上),然后生成了沿目标海岸线的行进时间图和最大水高剖面。千里马也被归入三级预期海啸威胁代码中。

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