Tsunami Hazard Evaluation of the Eastern Mediterranean: Historical Analysis and Selected Modeling

2007 ◽  
Vol 97 (3) ◽  
pp. 705-724 ◽  
Author(s):  
A. Salamon ◽  
T. Rockwell ◽  
S. N. Ward ◽  
E. Guidoboni ◽  
A. Comastri
Author(s):  
Mauricio Fuentes Serrano ◽  
Sebastián Riquelme Muñoz ◽  
Miguel Medina ◽  
Matias Mocanu ◽  
Rodrigo Filippi Fernandez

2012 ◽  
Vol 12 (1) ◽  
pp. 151-163 ◽  
Author(s):  
A. Grezio ◽  
P. Gasparini ◽  
W. Marzocchi ◽  
A. Patera ◽  
S. Tinti

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.


2011 ◽  
Vol 34 (1) ◽  
pp. 29-47 ◽  
Author(s):  
V. Ranga Rao ◽  
N. T. Reddy ◽  
J. Sriganesh ◽  
M. V. Ramana Murthy ◽  
Tad S. Murty

2017 ◽  
Vol 93 (S1) ◽  
pp. 127-152 ◽  
Author(s):  
Panon Latcharote ◽  
Khaled Al-Salem ◽  
Anawat Suppasri ◽  
Tanuspong Pokavanich ◽  
Shinji Toda ◽  
...  

2019 ◽  
Vol 7 (1) ◽  
pp. 111-155
Author(s):  
Nikolaus Leo Overtoom

Abstract Alexander the Great’s conquests ushered in the Hellenistic era throughout the ancient Mediterranean and Middle East. In this period, the Seleucids, one of most successful of the Successor dynasties, ruled over most of the Middle East at the height of their power. Yet two rising powers in the ancient world, Rome and Parthia, played a crucial role in the decline and eventual fall of the Seleucids. In a prior article, I argued that geopolitical developments around the Eastern Mediterranean in the middle third century BCE were indirectly responsible for the emergence of the Parthian state in Iran. Disastrous military conflicts at home and abroad in the west caused a sudden decline of Seleucid power in the 240s–230s, triggering what political scientists call a power-transition crisis. This article utilizes similar approaches to historical analysis and International Relations theory to contend that, after a period of recovery, a further sudden decline of Seleucid power in the 160s–130s triggered another power-transition crisis that brought an end to Seleucid hegemony over the Middle East permanently. The crisis facilitated the rapid transformation of the Parthian state from a minor kingdom to a major empire, drastically changing the international environment of the ancient world.


2021 ◽  
Vol 8 ◽  
Author(s):  
Amos Salamon ◽  
Eran Frucht ◽  
Steven N. Ward ◽  
Erez Gal ◽  
Marina Grigorovitch ◽  
...  

Unique geological and seismotectonic settings may trigger a multicascading hazard and should be identified beforehand. Such is the head of the Gulf of Elat–Aqaba (HGEA) at the northeastern end of the Red Sea where its geology, tectonics, bathymetry, and earthquake and tsunami history exhibit clear potential for earthquake and submarine-landslide tsunami generation. We thus investigated the possible tsunamigenic sources in the gulf and evaluated the resulting hazard at the HGEA. First, we assembled a bathymetric grid and adopted GeoClaw software to simulate most of the earthquake-tsunami scenarios. Next, we resolved the scheme of the largest possible tsunamigenic earthquakes along the deep basins of the Gulf of Elat (GEA) and the associated Dead Sea rift valley, as well as the potential tsunamigenic submarine landslides in the HGEA. The use of GeoClaw was verified against the 1995 tsunami generated by the Nuweiba Mw 7.2 earthquake, and then operated to simulate a suite of earthquake scenarios. Results showed that the marginal faults of Elat Basin pose the highest tsunami hazard to the Israeli part of the HGEA. To better assess that hazard, we screened the geology and seismotectonics of the HGEA and found that the Elat normal fault presents the worst-case scenario for Elat city. It is capable of generating a multicascading threat of earthquake and submarine-landslide tsunami, local subsidence that can increase inundation, and above all, destructive ground motion. Scenarios of a tsunami caused by the worst-case earthquake on the Elat fault simulated by GeoClaw and Ward’s (Tsunami, The encyclopedia of solid earth geophysics. 2011, 1473–1493) approach, and submarine landslide in the HGEA simulated by Wang et al.’s (Geophys. J. Int., 2015, 201, 1534–1544) ‘Tsunami Squares’ approach, demonstrated waves as high as 4 m along these coasts. Accordingly, we constructed a map of the evacuation zone. We also show that strong ground-shaking and retreat of the sea at the HGEA should be considered a tsunami warning, although false alarms are inevitable. Furthermore, tsunami hazard exists all along the gulf and further assessments are needed to quantify this hazard and increase awareness among the area's population.


Geomorphology ◽  
2016 ◽  
Vol 268 ◽  
pp. 197-206 ◽  
Author(s):  
Débora Beigt ◽  
Gustavo Villarosa ◽  
Eduardo A. Gómez ◽  
Carolina Manzoni

2011 ◽  
Vol 31 (7) ◽  
pp. 1080
Author(s):  
Nurcan Meral Ozel ◽  
Necmioglu Ocal ◽  
Yalciner Ahmet Cevdet ◽  
Kalafat Dogan ◽  
Erdik Mustafa

2020 ◽  
Vol 8 (11) ◽  
pp. 886
Author(s):  
Dimitrios-Vasileios Batzakis ◽  
Loukas-Moysis Misthos ◽  
Gerasimos Voulgaris ◽  
Konstantinos Tsanakas ◽  
Maria Andreou ◽  
...  

Santorini Island, located in the Southern Aegean Sea, is prone to tsunamis due to its proximity to the Hellenic subduction zone, which is one of the major tsunamigenic areas. Characteristic events, such as those of 365 A.D. and 1303 A.D. greatly affected the coasts of the Eastern Mediterranean Sea, causing significant loss of life and construction damage. Tsunami disaster risk is nowadays significantly higher due to the increased exposure of the buildings as a result of the economic and touristic growth of the Aegean Islands. This study focuses on the eastern coast of Santorini, since its morphology and human presence amplify the necessity to assess its building vulnerability. After conducting an exposure analysis at the settlements of the eastern coast, Kamari poses the highest physical, social and economic relative exposure to any potential natural hazard. The main objective of this research is to quantify the building stock’s vulnerability to tsunami hazard. For this purpose, a “worst-case run-up scenario” was developed. Considering the history of tsunamis in the Aegean Sea, an extreme sea-level rise after a 10 m a.s.l. tsunami run-up, caused by an earthquake with Mw~8.5, was assumed. The relative vulnerability of the buildings in Kamari was calculated via the application of the Papathoma Tsunami Vulnerability Assessment (PTVA-4) analytic model. The results indicate that 423 buildings are within the inundation zone, 58% of which are characterized as highly and very highly vulnerable to tsunamis, revealing the problematic characteristics of the building stock, offering important information to the decision-makers to mitigate a possible future tsunami impact.


Author(s):  
Mauricio Fuentes Serrano ◽  
Sebastián Riquelme Muñoz ◽  
Miguel Medina ◽  
Matias Mocanu ◽  
Rodrigo Filippi Fernandez

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