Laura Borzì, Pietro Scala, Salvatore Distefano, F. X. Anjar Tri Laksono, Giorgio Manno, Sara Innangi, Fabiano Gamberi, János Kovács, Giuseppe Ciraolo, Agata Di Stefano
{"title":"Tsunami propagation and flooding maps: An application for the Island of Lampedusa, Sicily Channel, Italy","authors":"Laura Borzì, Pietro Scala, Salvatore Distefano, F. X. Anjar Tri Laksono, Giorgio Manno, Sara Innangi, Fabiano Gamberi, János Kovács, Giuseppe Ciraolo, Agata Di Stefano","doi":"10.1002/esp.5996","DOIUrl":null,"url":null,"abstract":"<p>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 (M<sub>w</sub> 8.5, 7.5, 6.5) generated by hypothetical earthquakes in the Hellenic Arc. In the M<sub>w</sub> 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 M<sub>w</sub> 7.5 magnitude scenario demonstrates reduced flooded areas, with the cliffs containing the waves and preventing further flooding. Water depths and velocities in the M<sub>w</sub> 7.5 scenario remain minimal. Changes in both propagation and flooding are not significant between scenarios M<sub>w</sub> 7.5 and M<sub>w</sub> 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.</p>","PeriodicalId":11408,"journal":{"name":"Earth Surface Processes and Landforms","volume":"49 14","pages":"4842-4861"},"PeriodicalIF":2.8000,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/esp.5996","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth Surface Processes and Landforms","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/esp.5996","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
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.
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