Tsunami propagation and flooding maps: An application for the Island of Lampedusa, Sicily Channel, Italy

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Laura Borzì, Pietro Scala, Salvatore Distefano, F. X. Anjar Tri Laksono, Giorgio Manno, Sara Innangi, Fabiano Gamberi, János Kovács, Giuseppe Ciraolo, Agata Di Stefano
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引用次数: 0

Abstract

The Mediterranean coastlines are densely populated zones which host key socio-economic and commercial activities. For this reason, coastal areas are vulnerable sites in case of natural disasters as tsunamis that can strike coasts causing widespread damage to the population and facilities. For these reasons, several studies were performed over the last decade to study the impact of tsunami waves on the coasts. This research assessed the inundation risk due to a tsunami wave which can hit the southeastern coast of Lampedusa Island. The coastal low-lying geomorphological setting of the southeastern part of the island led to significant socio-economic growth, but Lampedusa falls within the Mediterranean Sea, a high-tsunamigenic area, therefore, the need to investigate tsunami propagation and coastal flooding of this sensitive site emerged. For this scope, a calculation chain model was implemented incorporating three steps: the DELFT-3D software for earthquake effects modelling, MIKE 21 Flow Model FM for nearshore propagation and HEC-RAS for onshore tsunami inundation modelling. The simulations illustrate the impact of three tsunami scenarios with different magnitudes (Mw 8.5, 7.5, 6.5) generated by hypothetical earthquakes in the Hellenic Arc. In the Mw 8.5 magnitude scenario, significant flooding occurs in the harbour region, with maximum water depths reaching approximately 3.5 m. The maximum water velocity in this scenario reaches about 15 m/s in the eastern portion, adjacent to cliffs impacted by the tsunami wave. In contrast, the Mw 7.5 magnitude scenario demonstrates reduced flooded areas, with the cliffs containing the waves and preventing further flooding. Water depths and velocities in the Mw 7.5 scenario remain minimal. Changes in both propagation and flooding are not significant between scenarios Mw 7.5 and Mw 6.5. This methodology can be employed for more accurate tsunami wave simulations not only in the Mediterranean region but also in various case studies.

Abstract Image

海啸传播和洪水地图:意大利西西里海峡兰佩杜萨岛的应用
地中海沿岸是人口稠密区,主要的社会经济和商业活动都在这里进行。因此,沿海地区在发生海啸等自然灾害时非常脆弱,海啸会袭击海岸,对居民和设施造成大面积破坏。因此,在过去的十年中进行了多项研究,以了解海啸波对海岸的影响。这项研究评估了可能袭击兰佩杜萨岛东南海岸的海啸波造成的淹没风险。兰佩杜萨岛东南部沿海低洼的地貌环境带来了显著的社会经济增长,但兰佩杜萨岛位于地中海,属于高海啸区,因此需要对这一敏感地区的海啸传播和沿海洪水进行研究。在这一范围内,实施了一个计算链模型,包括三个步骤:DELFT-3D 软件用于地震影响建模,MIKE 21 流量模型 FM 用于近岸传播,HEC-RAS 用于陆上海啸淹没建模。模拟结果显示了希腊弧地区假定地震引发的三种不同震级(8.5 级、7.5 级和 6.5 级)海啸的影响。在海啸威力为 8.5 级的情况下,港口地区会出现严重的洪水,最大水深约为 3.5 米。相比之下,在 7.5 级海啸情况下,由于悬崖挡住了海浪,防止了进一步的洪水泛滥,洪水淹没区域有所减少。7.5 级海啸的水深和流速仍然很小。7.5 级和 6.5 级地震的传播和洪水变化都不大。不仅在地中海地区,而且在各种案例研究中,都可以采用这种方法对海啸波进行更精确的模拟。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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