A shallow-flow model for the propagation of tsunamis over complex geometries and mobile beds

A distinguishable feature of overland tsunami propagation is the incorporation of solids within the flow column, either sediment from the natural environment or remains from built infrastructure. This article describes a 2DH (two-dimensional horizontal) mathematical model particularly suited for tsu...

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Bibliographic Details
Published inNatural hazards and earth system sciences Vol. 13; no. 10; pp. 2533 - 2542
Main Authors Conde, D. A. S, Baptista, M. A. V, Sousa Oliveira, C, Ferreira, R. M. L
Format Journal Article
LanguageEnglish
Published Katlenburg-Lindau Copernicus GmbH 16.10.2013
Copernicus Publications
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Summary:A distinguishable feature of overland tsunami propagation is the incorporation of solids within the flow column, either sediment from the natural environment or remains from built infrastructure. This article describes a 2DH (two-dimensional horizontal) mathematical model particularly suited for tsunami propagation over complex and dynamic geometries, such as river and estuarine mobile beds. The discretization scheme is based on a finite-volume method using a flux-splitting technique featuring a reviewed Roe-Riemann solver, with appropriate source-term formulations to ensure full conservativeness. The model is validated with laboratory data and paleo-tsunami evidence. As a forecasting application, it is applied to a tsunami scenario in the Tagus estuary, an effort justified by the numerous catastrophic tsunamis that are known to have struck this location over the past two millennia. The obtained results show that, despite the significant differences in Lisbon's layout and morphology, a 1755-like tsunami would still inflict a devastating impact on this major city.
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ISSN:1684-9981
1561-8633
1684-9981
DOI:10.5194/nhess-13-2533-2013