Tsunami risk assessments in Messina, Sicily – Italy

Abstract. We present a first detailed tsunami risk assessment for the city of Messina where one of the most destructive tsunami inundations of the last centuries occurred in 1908. In the tsunami hazard evaluation, probabilities are calculated through a new general modular Bayesian tool for Probability Tsunami Hazard Assessment. The estimation of losses of persons and buildings takes into account data collected directly or supplied by: (i) the Italian National Institute of Statistics that provides information on the population, on buildings and on many relevant social aspects; (ii) the Italian National Territory Agency that provides updated economic values of the buildings on the basis of their typology (residential, commercial, industrial) and location (streets); and (iii) the Train and Port Authorities. For human beings, a factor of time exposition is introduced and calculated in terms of hours per day in different places (private and public) and in terms of seasons, considering that some factors like the number of tourists can vary by one order of magnitude from January to August. Since the tsunami risk is a function of the run-up levels along the coast, a variable tsunami risk zone is defined as the area along the Messina coast where tsunami inundations may occur

A Methodology for a Comprehensive Probabilistic Tsunami Hazard Assessment: Multiple Sources and Short-Term Interactions

We propose a methodological approach for a comprehensive and total probabilistic tsunami hazard assessment (TotPTHA), in which many different possible source types concur to the definition of the total tsunami hazard at given target sites. In a multi-hazard and multi-risk perspective, the approach allows us to consider all possible tsunamigenic sources (seismic events, slides, volcanic eruptions, asteroids, etc.). In this respect, we also formally introduce and discuss the treatment of interaction/cascade effects in the TotPTHA analysis and we demonstrate how the triggering events may induce significant temporary variations in short-term analysis of the tsunami hazard. In two target sites (the city of Naples and the island of Ischia in Italy) we prove the feasibility of the TotPTHA methodology in the multi-source case considering near submarine seismic sources and submarine mass failures in the study area. The TotPTHA indicated that the tsunami hazard increases significantly by considering both the potential submarine mass failures and the submarine seismic events. Finally, the importance of the source interactions is evaluated by applying a triggering seismic event that causes relevant changes in the short-term TotPTHA

Tsunami hazards in the Catalan Coast, a low-intensity seismic activity area

The final publication is available at Springer via http://dx.doi.org/10.1007/s11069-017-2918-zThe potential impacts of tsunamis along the Catalan Coast (NW Mediterranean) are analysed using numerical modelling. The region is characterized by moderate to low seismic activity and by moderate- to low-magnitude earthquakes. However, the occurrence of historical strong earthquakes and the location of several active offshore faults in front of the coast suggest that the possibility of an earthquake-triggered tsunami is not negligible although of low probability. Up to five faults have been identified to generate tsunamis, being the highest associated possible seismic magnitudes of up to 7.6. Coastal flooding and port agitation are characterized using the Worst-case Credible Tsunami Scenario Analysis approach. The results show a multiple fault source contribution to tsunami hazard. The shelf dimensions and the existence of submerged canyons control the tsunami propagation. In wide shelves, waves travelling offshore may become trapped by refraction causing the wave energy to reach the coastline at some distance from the origin. The free surface water elevation increases at the head of the canyons due to the sharp depth gradients. The effects of potential tsunamis would be very harmful in low-lying coastal stretches, such as deltas, with a high population concentration, assets and infrastructures. The Ebro delta appears to be the most exposed coast, and about the 20% of the delta surface is prone to flooding due to its extremely low-lying nature. The activity at Barcelona port will be severely affected by inflow backflow current at the entrance of up to 2 m/s.Peer ReviewedPostprint (author's final draft

Data assimilation of temperature and salinity profiles in the Adriatic Sea regional model

Temperature and salinity data collected during the October 2002- October 2003 period have been assimilated into a version of the Princeton Ocean Model implemented over the entire Adriatic Sea. The scheme used is SOFA (System for Ocean Analysis and Forecast, DE MEY & BENKIRAN, 2002) and this is the first coastal application of this scheme. The CTD data were collected in 4 coastal areas (Emilia – Romagna Coastal strip, the Gulf of Trieste, the Rovinj and Pelješac-Vis-Drvenik coastal strips) while temperature profiles were acquired with XBT in the southern Adriatic Sea deep ocean areas. The analysis skill scores are examined in order to evaluate the assimilation performance. The results of the assimilation are first compared with independent analyses of satellite Sea Surface Temperature (SST) and it is found that assimilation of profiles improves the SST model estimate. Furthermore, the Root Mean Square (RMS) difference between model and temperature and salinity profiles before data insertion is analysed. The range of RMS temperature error is less than 1 0C for the entire area and decreases with time, indicating a positive impact of the assimilation. The RMS of salinity is less than 1 psu and it also shows a decreasing trend during the assimilation period.Published149-168ope

Data assimilation of temperature and salinity profiles in the Adriatic Regional Model

Temperature and salinity data collected during the October 2002- October 2003 period have been assimilated into a version of the Princeton Ocean Model implemented over the entire Adriatic Sea. The scheme used is SOFA (System for Ocean Analysis and Forecast, DE MEY & BENKIRAN, 2002) and this is the first coastal application of this scheme. The CTD data were collected in 4 coastal areas (Emilia – Romagna Coastal strip, the Gulf of Trieste, the Rovinj and Pelješac-Vis-Drvenik coastal strips) while temperature profiles were acquired with XBT in the southern Adriatic Sea deep ocean areas. The analysis skill scores are examined in order to evaluate the assimilation performance. The results of the assimilation are first compared with independent analyses of satellite Sea Surface Temperature (SST) and it is found that assimilation of profiles improves the SST model estimate. Furthermore, the Root Mean Square (RMS) difference between model and temperature and salinity profiles before data insertion is analysed. The range of RMS temperature error is less than 1 0C for the entire area and decreases with time, indicating a positive impact of the assimilation. The RMS of salinity is less than 1 psu and it also shows a decreasing trend during the assimilation period.Published149-168ope

A Bayesian procedure for Probabilistic Tsunami Hazard Assessment

In this paper, a Bayesian procedure is implemented for the Probability Tsunami Hazard Assessment (PTHA). The approach is general and modular incorporating all significant information relevant for the hazard assessment, such as theoretical and empirical background, analytical or numerical models, instrumental and historical data. The procedure provides the posterior probability distribution that integrates the prior probability distribution based on the physical knowledge of the process and the likelihood based on the historical data. Also, the method deals with aleatory and epistemic uncertainties incorporating in a formal way all sources of relevant uncertainty, from the tsunami generation process to the wave propagation and impact on the coasts. The modular structure of the procedure is flexible and easy to modify and/or update as long as new models and/or information are available. Finally, the procedure is applied to an hypothetical region, Neverland, to clarify the PTHA evaluation in a realistic case. © Springer Science+Business Media B.V. 2009

A Bayesian procedure for Probabilistic Tsunami Hazard Assessment

In this paper, a Bayesian procedure is implemented for the Probability Tsunami Hazard Assessment (PTHA). The approach is general and modular incorporating all significant information relevant for the hazard assessment, such as theoretical and empirical background, analytical or numerical models, instrumental and historical data. The procedure provides the posterior probability distribution that integrates the prior probability distribution based on the physical knowledge of the process and the likelihood based on the historical data. Also, the method deals with aleatory and epistemic uncertainties incorporating in a formal way all sources of relevant uncertainty, from the tsunami generation process to the wave propagation and impact on the coasts. The modular structure of the procedure is flexible and easy to modify and/or update as long as new models and/or information are available. Finally, the procedure is applied to an hypothetical region, Neverland, to clarify the PTHA evaluation in a realistic case

Il clima che cambia, se cambia

Del clima e dei suoi cambiamenti si parla moltissimo. Naturalmente anche a Bologna il clima ha subito vari mutamenti nel tempo. Sapevate che la nostra città ha avuto la sua piccola “età glaciale” nel Medioevo, culminata nei primi anni dell’800? Nell’inverno 1829-30 nevicò per trecento ore di seguito (più di dodici giorni) e nelle piazze si raccolsero cumuli di neve alti fino a venti metri. Pensate che meravigliosi pupazzi di neve si sarebbero potuti costruire! Chi di voi si ricorda di grandi nevicate in città? Nessuno, perché non ci sono più da diversi anni. Ma cos’è il clima? Quali sono le cause delle sue trasformazioni? Cosa fa il climatologo? Il percorso attivo proposto in questa occasione, insieme ai libri che la biblioteca propone in questa pubblicazione, aiuta a orientarci in una questione complessa sulla quale spesso si dicono cose inesatte quando non proprio scorrette. Attraverso esperimenti e giochi, capiremo come funziona la macchina del clima; scopriremo cos'è l’effetto serra e in che modo lo sfruttamento di certe risorse e la produzione di CO2 da parte dell'uomo influiscano sul clima. Cercheremo di comprendere i rischi del nostro pianeta e le possibilità future. Partendo proprio noi, dai nostri comportamenti quotidiani, dalle piccole azioni che ciascuno può compiere per controllare i cambiamenti climatici. Nei libri possiamo esplorare i deserti, le foreste, i mari e gli oceani dove il clima varia notevolmente e quindi variano gli animali e la vegetazione, capire il meccanismo delle stagioni, la meteorologia, i fenomeni atmosferici, imparare i comportamenti da tenere, le cose da fare per proteggere la terra e i suoi abitanti. Quando da grandi usciremo di casa, saliremo su un autobus o su una barca in mezzo a una nuvola di fastidiosi insetti? Sta a noi cercare le informazioni giuste per prenderci cura del nostro futuro. Biblioteca Sala Borsa Ragazz

Dynamical budgets of the Antarctic Circumpolar Current using ocean general-circulation models

Three general-circulation models (FRAM, OCCAM and POP) are used to investigate the dynamics of the Antarctic Circumpolar Current (ACC) at the latitudes of the Drake Passage where the ACC is unbounded. In these general circulation models, bottom form stress balances the wind stress in the momentum budgets. In the vorticity budgets, the main balance is between wind curl and bottom pressure torque in FRAM, OCCAM and POP. Moreover, in the ACC belt all topographic features are regions of nonlinearity and bottom pressure torque variations, with the Drake Passage playing the largest role. Transient eddy Reynolds stresses (TERSs) play a different role in the three models. In the upper levels, TERSs accelerate the flow in the POP and FRAM models, but decelerate the flow in OCCAM. The behaviour of TERSs change throughout the whole water column in the ACC belt and Reynolds stresses have a dragging effect on the flow below the levels where the topography starts to obstruct the flow. The total volume transport in three models is very different. Additionally, the different spatial resolution, which results in a different level of eddy kinetic energy, has a significant influence on the transport

Il clima che cambia, se cambia

Del clima e dei suoi cambiamenti si parla moltissimo. Naturalmente anche a Bologna il clima ha subito vari mutamenti nel tempo. Sapevate che la nostra città ha avuto la sua piccola “età glaciale” nel Medioevo, culminata nei primi anni dell’800? Nell’inverno 1829-30 nevicò per trecento ore di seguito (più di dodici giorni) e nelle piazze si raccolsero cumuli di neve alti fino a venti metri. Pensate che meravigliosi pupazzi di neve si sarebbero potuti costruire! Chi di voi si ricorda di grandi nevicate in città? Nessuno, perché non ci sono più da diversi anni. Ma cos’è il clima? Quali sono le cause delle sue trasformazioni? Cosa fa il climatologo? Il percorso attivo proposto in questa occasione, insieme ai libri che la biblioteca propone in questa pubblicazione, aiuta a orientarci in una questione complessa sulla quale spesso si dicono cose inesatte quando non proprio scorrette. Attraverso esperimenti e giochi, capiremo come funziona la macchina del clima; scopriremo cos'è l’effetto serra e in che modo lo sfruttamento di certe risorse e la produzione di CO2 da parte dell'uomo influiscano sul clima. Cercheremo di comprendere i rischi del nostro pianeta e le possibilità future. Partendo proprio noi, dai nostri comportamenti quotidiani, dalle piccole azioni che ciascuno può compiere per controllare i cambiamenti climatici. Nei libri possiamo esplorare i deserti, le foreste, i mari e gli oceani dove il clima varia notevolmente e quindi variano gli animali e la vegetazione, capire il meccanismo delle stagioni, la meteorologia, i fenomeni atmosferici, imparare i comportamenti da tenere, le cose da fare per proteggere la terra e i suoi abitanti. Quando da grandi usciremo di casa, saliremo su un autobus o su una barca in mezzo a una nuvola di fastidiosi insetti? Sta a noi cercare le informazioni giuste per prenderci cura del nostro futuro. Biblioteca Sala Borsa RagazziPublished5.7. TTC - Biblioteche ed editoria5.8. TTC - Formazione e informazioneope