In this work we review the impact of potential tsunamigenic events on the Suez Canal by means of numerical hydrodynamic simulations. To do this we selected three possible seismic sources affecting the area of study and able to trigger tsunami, two of which located in the eastern Mediterranean region and one in the Gulf of Aqaba. The selected sources reviewed and characterized to provide the input to the hydrodynamic analysis are the Lebanon Thrust Fault, two fault segments of the Cyprus Arc and the Evrona and Elat faults (Dead Sea Fault system).
Tsunami event due to Lebanon Thrust Fault impacts the Nile Delta and propagates into the Suez Canal with the formation of long sub waves with a maximum water level reached at Port Said after 2 hours and a half from the beginning of propagation.
Tsunami generated by seismic events due to major fault systems belonging to the Cyprus Arc affect Port Said with a maximum water level reached at about 3 hours and a half after the seismic event.
Finally, simulations developed considering as seismic source the Evrona Dead Sea Fault, located in the Gulf of Aqaba, reveal that a significant water level increase is observed along the entire Canal at about six hours from the beginning of the tsunamigenic event.