Tsunami modelling and prediction

Tsunamis (large waves formed by huge and sudden displacements) are a secondary effect of geological events like

• rock slides and rock falls into fjords and lakes
• submarine landslides
• earthquakes

A tsunami devestated Japan after the earthquake 11. March 2011

Tsunami events in Norway are most often due to rock slides. Other triggering mechanisms are relevant because they generate similar hazards and require similar solution approaches. Tsunamis have been reported since ancient times and have caused thousands of deaths and severe destruction worldwide. They are of major interest internationally. Selected examples comprise:

• The 11 March 2011 Tohoku tsunami, Japan (earthquake Mw 9.0)
• The 26 December 2004 Indian Ocean  tsunami (earthquake Mw 9.3) caused 200,000 - 300,000 casualties
• In the 1990's, four tsunamis ravaged the coast of Nicaragua, Indonesia, Japan and Papua New Guinea causing loss of about 4 000 lives. 
• In Norway, the three most severe events, leading to the deaths of 174 people altogether, did all occur in the twentieth century (Loen 1905, 1936; Tafjord 1934).
• The submarine Storegga Slide on the Norwegian Continental Slope has been identified as responsible for huge tsunamis affecting Norway, Scotland and the other European Coasts in Holocene times.
  

The tsunami generated by the Tohoku earthquake 11. March 2011. Maximum surface elevation in meter.

Hence, tsunamis constitute a serious natural hazard for the environment and populations in exposed areas. Future catastrophes can be mitigated or prevented by tsunami hazard assessment based on statistics and geological analysis, by risk analyses based on studies of landslide dynamics, tsunami propagation and coastal impact, and by various tsunami mitigation measures. Moreover, tsunami predictions are fundamental in engineering design and location of coastal installations, dams, submerged bridges, offshore constructions, aquaculture, etc.

Scientific objectives
The project has the following main goals:

• Produce general and powerful tools for tsunami modelling and combine these tools in a general domain decomposition framework.
• Investigate hydrodynamic models to establish the limitations of current tsunami models and to test their sensitivity to the input parameters.
• Undertake comprehensive scientific investigation of the performance of domain decomposition and parallel computing in a tsunami context.
• Establish operational hydrodynamic models for tsunamis and tsunami generation with coupling to the geological trigger.
• Improve the status of operational tsunami modelling at NGI and other Norwegian institutions.
• Perform important case studies on tsunamis.
• ¿ Establish criteria for landslide and tsunami hazard and risk evaluation in Norway, considering potential for and consequences of release for different triggers and various types of landslides; develop landslide and tsunami hazard and risk mapping procedures.