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Source mechanisms of volcanic tsunamis.
Paris, Raphaël (2015) Source mechanisms of volcanic tsunamis. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 373 (20140380). DOI 10.1098/rsta.2014.0380.
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Abstract
Volcanic tsunamis are generated by a variety of mechanisms, including volcano-tectonic earthquakes, slope instabilities, pyroclastic flows, underwater explosions, shock waves and caldera collapse. In this review, we focus on the lessons that can be learnt from past events and address the influence of parameters such as volume flux of mass flows, explosion energy or duration of caldera collapse on tsunami generation. The diversity of waves in terms of amplitude, period, form, dispersion, etc. poses difficulties for integration and harmonization of sources to be used for numerical models and probabilistic tsunami hazard maps. In many cases, monitoring and warning of volcanic tsunamis remain challenging (further technical and scientific developments being necessary) and must be coupled with policies of population preparedness.
Document Type: | Article |
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Keywords: | volcanic tsunami, flank instability, pyroclastic flows, caldera collapse, underwater explosions |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Royal Society of London |
Projects: | Enrichment, ASTARTE |
Date Deposited: | 25 Jul 2017 08:52 |
Last Modified: | 12 Jun 2020 10:38 |
URI: | https://oceanrep.geomar.de/id/eprint/38896 |
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