The simulations run on the North-East Atlantic model show the evolution of relatively well 
resolved signals, 35 grid points per single signal at 4,000 m depth, and still about 15 grid 
points per single signal at 1,000 m depth. The area covered by the model (Fig. 7.2.0) 
includes the continental slope and the shelf. In both areas, tsunami are subject to strong 
modification. 
46 
15 i 
-10 J— —^ ^ 
00:00:00 01:00:00 02:00:00 03:00:00 
Fig. 7.1.2: Water level evolution in Bergen using different wave height input signals 
(3 positive single waves, period 1800 s, North Sea model 2 km). 
Fig. 7.1.3: Water level evolution in Lerwick using different wave height input signals 
(3 positive single waves, period 1800 s, North Sea model 2 km) 
7.2 North-East Atlantic Ocean