IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps | Infrastructure
[ report an error in this record ]basket (0): add | show Print this page

Source mechanisms of volcanic tsunamis
Paris, R. (2015). Source mechanisms of volcanic tsunamis. Philos. Trans. - Royal Soc., Math. Phys. Eng. Sci. 373(2053): 20140380. https://dx.doi.org/10.1098/rsta.2014.0380
In: Philosophical Transactions - Royal Society. Mathematical, Physical and Engineering Sciences. Royal Society: London. ISSN 1364-503X; e-ISSN 1471-2962, more
Peer reviewed article  

Available in  Author 

Keyword
    Marine/Coastal

Author  Top 
  • Paris, R.

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.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Author