Abstract

The 2015 Illapel earthquake (Mw 8.3) generated a tsunami that significantly impacted the central-north Chilean coast. Previous studies have utilized numerical modelling to analyse this tsunami propagation, yet none have applied a comparative forward and inverse modelling approach to accurately estimate the earthquake source parameters, flow characteristics and sediment transport. A forward model TELEMAC was employed to simulate tsunami hydrodynamics and sediment transport, calibrating it against tide gauge records to identify the most accurate earthquake source scenario. Simultaneously, the inverse model TSUFLIND was utilized to deduce hydrodynamic properties during the inundation phase from sediment deposit characteristics. The performance of the models was evaluated by comparing flow characteristics. The approach was tested along the Tongoy estuary by comparing it against regional tide gauge data, alongside measurements of flow depth and run-up, and sediment deposit observations from five pits along the river (680 m to 1280 m inland). Along the five pits, TELEMAC results indicate the tsunami flow depths ranged between 3.22 m to 0.47 m, and onshore velocities ranged from 4.9 m/s to 2.21 m/s, with sediment deposition from 20 cm to 7 cm. On the other hand, TSUFLIND results were consistent with TELEMAC, with flow depths between 3.22 m to 0.68 m, velocities between 4.84 m/s to 2.05 m/s, and deposition thickness of 15 cm to 0.5 cm along the five pits. The agreement of the hydrodynamic results from both models highlights the importance of integrating geological evidence with numerical modelling where tide records or other hydrodynamic information cannot be obtained for tsunami events, highlighting the significance of a combined approach for advancing the understanding of tsunami hazards.