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TSUNAMI DAMAGE IN SOLOMON ISLANDS IN APRIL 2007 
 
Takashi Tomita, Port and Airport Research Institute, tomita@pari.go.jp 
Taro Arikawa, Port and Airport Research Institute, arikawa@pari.go.jp 
Daisuke Tatsumi, Port and Airport Research Institute, tatsumi@pari.go.jp 
Kazuhiko Honda, Port and Airport Research Institute, honda@pari.go.jp 
 
INTRODUCTION 
A tsunami following a M8.1 earthquake caused serious 
disasters in western islands of the Solomon Islands on 1 
April 2007 in UTC. The tsunami destroyed some coastal 
villages and killed 52 people according to the report of the 
government of the Solomon Islands on 30 April 2007. A 
post tsunami field survey was conducted in Simbo Island, 
Ghizo Island, Ranongga Islands, Vella Lavella Island and 
New Georgia Island near the epicenter for understanding 
of tsunami damages and characteristics of the striking 
tsunami.  
 
PROCEDURE OF FIELD SURVEY 
In the field survey, tsunami inundation heights and runup 
heights were measured from the level of sea surface at 
time of each measurement, and were converted to the 
heights above the estimated level of sea surface at the 
time the tsunami struck. Information on tsunami arrival 
time, the number of tsunami waves, scene of tsunami 
striking and people’s activity when the tsunami struck 
were gathered from residents and others. 
 
RESULTS OF FIELD SURVEY 
Figure 1 indicates tsunami inundation and runup heights 
measured in the field survey. The highest runup in our 
survey is 9.0 m in Tapurai, Simbo Island, which is in the 
subsidence area by the earthquake (Fritz and Kalligeris, 
2008). The tsunami inundation height is approximately 4-
5 m at the north part of Simbo Island and at the south 
coast of Ghizo Island, which suffer severe damages. On 
the contrary, tsunami inundation heights of 2 m or less 
are at the east coast of the south part of Vella Lavella 
Island where there are reefs in the offshore of the coast, 
and at the north coast of the east part of Ghizo Island 
which locates on the back side of the island against the 
tsunami incident direction.  
 
NUMERICAL SIMULATION 
Numerical simulations are carried out and compared to 
the survey results. The bathymetric data is based on 1-
minute grid data of GEBCO and a nautical chart around 
Ghizo Island. The minimum grid size of calculation is 200 
m around the southern coast of Ghizo Island. Conducting 
numerical simulations based on several fault models, 
Tanioka’s model is finally selected, which is determined 
from the results of ground uplift and subsidence by the 
earthquake. 
 
In the numerical simulations, the tsunami is trapped 
around the islands near the epicenter and hardly 
propagated behind the islands. Especially the high 
tsunami appears around overall of Simbo Island and the 
southern coast of Ghizo Island. 
 
Comparison of calculated tsunami heights with the 
inundation and runup heights measured in the field 
survey is indicated in Figure 2. The calculation results are 
good agreement with the survey results in the locations 
where there are less developing coral reefs in front of 
coasts. However, in Munda, Vonunu, Titiana and New 
Manra, the numerical results are larger than the survey 
results, because the coral reefs develop in physical 
places but no or narrow reefs are in the calculation.  
 
MITIGATION OF TSUNAMI DISASTERS 
Human lives were saved by evacuation to hills near 
coasts. In fact, several residents ran to the hills after they 
looked at the tsunami coming in the offshore. High-floored 
houses with stilts also saved human lives as well as 
reduce tsunami destruction rate in the area. These facts 
indicate importance of vertical evacuation. 
 
 
 
Figure 1 - Measured tsunami inundation and runup 
heights (    : Inundation height,    : Runup height) 
 
 
 
Figure 2 – Comparison between measured tsunami trace 
heights and calculated tsunami heights 
 
REFERENCES 
Fritz and Kalligeris (2008): Ancestral heritage saves tribes 
during 1 April 2007 Solomon Islands tsunami, GRS, 35. 
Hamburg, August 31st to September 5th, 2008
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