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The influence of landslide shape and continental shelf on landslide generated tsunamis along a plane beach

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posted on 2015-03-26, 15:59 authored by Emiliano Renzi, Paolo Sammarco
This work proposes an advancement in analytical modelling of landslide tsunamis propagating along a plane beach. It is divided into two parts. In the first one, the analytical two-horizontal-dimension model of Sammarco and Renzi (2008) for tsunamis generated by a Gaussian-shaped landslide on a plane beach is revised and extended to realistic landslide shapes. The influence of finiteness and shape of the slide on the propagating waves is investigated and discussed. In the second part, a new model of landslide tsunamis propagating along a semi-plane beach is devised to analyse the role of the continental platform in attenuating the wave amplitude along the shoreline. With these parameters taken into account, the fit with available experimental data is enhanced and the model completed.

Funding

This work was funded by the Italian Ministry of Research (MIUR) under the research project “Development and validation of hydraulic and geologic tools for supporting a Tsunami Early Warning System. Implementation to the Stromboli (Eolie) landslide case” (PRIN-2007).

History

School

  • Science

Department

  • Mathematical Sciences

Published in

NATURAL HAZARDS AND EARTH SYSTEM SCIENCES

Volume

12

Issue

5

Pages

1503 - 1520 (18)

Citation

RENZI, E. and SAMMARCO, P., 2012. The influence of landslide shape and continental shelf on landslide generated tsunamis along a plane beach. Natural Hazards and Earth System Sciences, 12 (5), pp. 1503 - 1520.

Publisher

Copernicus Publications on behalf of European Geosciences Union / © The Authors

Version

  • VoR (Version of Record)

Publisher statement

This work is made available according to the conditions of the Creative Commons Attribution 3.0 Unported (CC BY 3.0) licence. Full details of this licence are available at: http://creativecommons.org/licenses/by/3.0/

Publication date

2012

Notes

This article was published by Copernicus Publications on behalf of the European Geosciences Union. It is an Open Access article distributed under the Creative Commons Attribution 3.0 Licence.

ISSN

1561-8633

Language

  • en

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