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  5. Risk communication about tsunamis in the Mediterranean Sea: challenges and pitfalls.
 
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Risk communication about tsunamis in the Mediterranean Sea: challenges and pitfalls.

Author(s)
Cerase, Andrea  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Type
Conference paper
Language
English
Obiettivo Specifico
1SR. TERREMOTI - Servizi e ricerca per la Società
Status
Published
Journal
2018 EGU General Assembly  
Date Issued
April 12, 2018
Conference Location
Austria Center Vienna (ACV), Wien (Osterreich)
URI
https://www.earth-prints.org/handle/2122/12280
Subjects
05.03. Educational, History of Science, Public Issues
05.08. Risk  
Subjects

risk communication

risk perception

tsunami

awareness

last mile

early warning

media

Abstract
According to a deep-rooted conviction, the occurrence of a tsunami in the Mediterranean Sea would bevery rare. Unfortunately, this belief is definitely false: at least 2,000 of the 80,000 victims of the great earthquakein Messina (1908) were due to the tsunami that followed earthquake (Boschi et al. 1995). In 1956, a 7.7 magnitudeearthquake close to the Cycladic island of Amorgos (Greece) triggered large waves that also hit coasts of Amorgos,Astypalaia and Folegandros, with run-up values of 30, 20, and 10 mt(Okal et al., 2009).More recently, in 2003 a relatively small tsunami caused by a 6.9 magnitude earthquake in Boumerdes (Algeria)hit the Western Mediterranean coast causing damage properties in at least eight harbours in Balearic Islands (Velaet al. 2011) and two little tsunamis occurred in Dodecanese respectively in 2016 and 2017.Such events, that are just a little part of the over 290 historically known events occurred in the Mediterranean(Maramai, Brizuela & Graziani, 2014) should remind geoscientists that 1) tsunami hazard is everything butimpossible and 2) tsunami come in all shapes and colours, and even a small event can result in serious damagesand loss of lifes. In such a scenario, risk communication about Mediterranean Tsunami is a challenging enterprise.According to Astarte project, which investigated people’s knowledge, preparedness and attitudes to cope withTsunami within six test sites across different nations, people have little knowledge about tsunamis, are likely tounderestimate both probability and consequences of such events, and their understanding is significantly affectedby media coverage (and social imagery) of big events such as the 2004 Sumatra Tsunami and the 2011 TohokuTsunami (Astarte, 2014).In such a scenario, where low probability and high uncertainty match with poor knowledge and familiaritywith tsunami hazard, risk communicators should avoid undue assumptions about public’s supposed attitudesand preparedness, that may results in serious consequences for the exposed population, geoscientists, and civilprotection officers. Hence, scientists must carefully shape their messages and rely on well-researched principledpractices rather on good intuition (Bostrom, & Löfstedt, 2003).For these reasons, the Centro Allerta Tsunami of the Istituto Nazionale di Geofisica e Vulcanologia, to ground aneffective science communication strategy, promoted a survey to investigate tsunami’s risk perception in two pilotregions of southern Italy, as to represent about 3.2mln people living in 183 coastal municipalities.The research is based on a sample of > 1000 people, organized into six main sections: socio-demographic dataand information on respondents’ territory; knowledge and sources of information on tsunami risk; contextualperception of risk posed by tsunamis; social representations of tsunami; role of cultural attitudes and worldviews; messages and channels to be used for tsunami early warning.Interviews will be administered within the end of February 2018, first data will be presented and discussed in this session.
References
Astarte (2014) Deliverable 9.7 Report on preparedness skills, resources and attitudes within the communities
Boschi, E., Ferrari, G., Gasperini, P., Guidoboni, E., Smriglio, G., & Valensise, G. (1995). Catalogo dei forti terremoti in Italia dal 461 aC al 1980. Istituto Nazionale di Geofisica.
Bostrom, A., & Löfstedt, R. E. (2003). Communicating risk: Wireless and hardwired. Risk analysis, 23(2), 241-248.
Maramai A., Brizuela B., Graziani L. – The Euro-Mediterranean Tsunami Catalogue, Annals of Geophysics, 57, 4, 2014, S0435; doi:10.4401/ag-6437
Okal, E. A., Synolakis, C. E., Uslu, B., Kalligeris, N., & Voukouvalas, E. (2009). The 1956 earthquake and tsunami in Amorgos, Greece. Geophysical Journal International, 178(3), 1533-1554.
Vela, J., Pérez, B., González, M., Otero, L., Olabarrieta, M., Canals, M., & Casamor, J. L. (2011). Tsunami resonance in the Palma de Majorca bay and harbour induced by the 2003 Boumerdes-Zemmouri algerian earthquake (Western Mediterranean). Coastal Engineering Proceedings, 1(32), 7.
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