Abstract

Destructive tsunamis are most often generated by large earthquakes occurring at subduction interfaces, but also other “atypical” sources—defined as crustal earthquakes and non-seismic sources altogether—may cause significant tsunami threats. Tsunamis may indeed be generated by different sources, such as earthquakes, submarine or coastal landslides, volcano-related phenomena, and atmospheric perturbations. The consideration of atypical sources is important worldwide, but it is especially prominent in complex tectonic settings such as the Mediterranean, the Caribbean, or the Indonesian archipelago. The recent disasters in Indonesia in 2018, caused by the Palu-Sulawesi magnitude Mw 7.5 crustal earthquake and by the collapse of the Anak-Krakatau volcano, recall the importance of such sources. Dealing with atypical sources represents a scientific, technical, and computational challenge, which depends on the capability of quantifying and managing uncertainty efficiently and of reducing it with accurate physical modelling. Here, we first introduce the general framework in which tsunami threats are treated, and then we review the current status and the expected future development of tsunami hazard quantifications and of the tsunami warning systems in Italy, with a specific focus on the treatment of atypical sources. In Italy, where the memory of historical atypical events like the 1908 Messina earthquake or the relatively recent 2002 Stromboli tsunami is still vivid, specific attention has been indeed dedicated to the progressive development of innovative strategies to deal with such atypical sources. More specifically, we review the (national) hazard analyses and their application for coastal planning, as well as the two operating tsunami warning systems: the national warning system for seismically generated tsunamis (SiAM), whose upstream component—the CAT-INGV—is also a Tsunami Service Provider of the North-eastern Atlantic, the Mediterranean and connected seas Tsunami Warning System (NEAMTWS) coordinated by the Intergovernmental Coordination Group established by the Intergovernmental Oceanographic Commission (IOC) of UNESCO, and the local warning system for tsunamis generated by volcanic slides along the Sciara del Fuoco of Stromboli volcano. Finally, we review the state of knowledge about other potential tsunami sources that may generate significant tsunamis for the Italian coasts, but that are not presently considered in existing tsunami warning systems. This may be considered the first step towards their inclusion in the national tsunami hazard and warning programs.

Highlights

  • A tsunami is a series of gravity waves propagating in the water and generated by its sudden large-scale displacement due to one external source [1]

  • The Palu-Sulawesi tsunami was generated by a magnitude Mw 7.5 crustal earthquake with a strike-slip source mechanism and with the possible contribution of landslides mobilized by the seismic shaking inside the Palu bay [4–6]; the Sunda Strait tsunami was instead generated by the collapse of the volcano edifice of Anak Krakatau, a volcanic island between Sumatra and Java islands [7–10]

  • The upstream component of the seismically generated tsunamis (SiAM), the CAT-INGV (Centro Allerta Tsunami of INGV; http://www.ingv.it/cat/it/, [110, 111]) is a Tsunami Service Providers (TSPs) (Tsunami Service Provider) of the North-eastern Atlantic, the Mediterranean and connected seas Tsunami Warning System (NEAMTWS), coordinated by the Intergovernmental Coordination Group established by the Intergovernmental Oceanographic Commission of UNESCO

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Summary

Introduction

A tsunami is a series of gravity waves propagating in the water and generated by its sudden large-scale displacement due to one external source [1]. Tsunamis generated by atypical sources are usually more local and probably less frequent than subduction zone events worldwide, and their effective hazard is more difficult to constrain, and it is often neglected [11, 17] Their forecasting in near-real-time for early warning purposes is rather challenging and not yet a well-established practice, as far as non-seismic sources are concerned. Coastal planning for SiAM is defined considering non-subduction zone earthquakes, being based on a regional PTHA including them [31, 51–53, 62, 63] Another local warning system is dedicated to tsunamis generated by collapses occurring within the volcanic system of Stromboli. We outline the potential scientific paths toward the improvement of the efficiency and the source coverage of the tsunami warning service (Sect. 6)

Probabilistic tsunami hazard analysis and tsunami forecast for warning
Tsunami generation and propagation models
Tsunami generation models
Tsunami propagation and inundation models
Tectonic setting of the Mediterranean region
Tsunami warning for earthquake-generated tsunamis
Hazard quantification
Italian Tsunami Warning System for seismically-induced tsunamis
Evacuation zones and civil protection coastal planning
Ongoing developments
Toward a national S-PTHA
Toward a tsunami warning based on real-time probabilistic tsunami forecast
Improving civil protection coastal planning
Tsunami warning at Stromboli volcano
Tsunami early-warning system at Stromboli
The multi-parametric monitoring network and tsunami warning
The elastic beacons (MEDA)
Tsunami detection
The acoustic warning system
Modelling of the 2019 events
Warning system
Other non-seismic tsunami sources in Italy
Ligurian Sea
Ischia and the Gulf of Naples (IGN)
Southern Tyrrhenian Sea Mounts (STSM)
Aeolian Archipelago (AA)
Western Calabria Margin (WCM)
Eastern Calabria Margin (ECM)
Eastern Sicily (ES): Messina Straits
Eastern Sicily (ES): Mount Etna
Eastern Sicily (ES): Hyblean-Malta Escarpment
Gela Margin (GM) and Sicily Channel (SC)
Adriatic Sea
Meteotsunamis
Outlook
Full Text
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