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Numerical modeling of the September 13, 1999 landslide and tsunami on Fatu Hiva Island (French Polynesia)
Author(s) -
Hébert Hélène,
Piatanesi Alessio,
Heinrich Philippe,
Schindelé François,
Okal Emile A.
Publication year - 2002
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2001gl013774
Subject(s) - subaerial , geology , cliff , landslide , bay , submarine landslide , seismology , oceanography , tsunami wave , submarine , bathymetry , geomorphology , paleontology
On September 13, 1999, Omoa Bay (Fatu Hiva Island, French Polynesia) was struck by 2 to 5 m high water waves: several buildings were flooded and destroyed but no lives were lost. Observations gathered during a post‐event survey revealed the recent collapse into the sea of a 300 × 300 m 2 , at least 20‐m thick, cliff located 5 km southeast of Omoa. This cliff failure most certainly triggered the tsunami waves since the cliff was reported intact 45 min earlier. We simulate the tsunami generation due to a subaerial landslide, using a finite‐difference model assimilating the landslide to a flow of granular material. Numerical modeling shows that a 0.0024‐km 3 landslide located in the presumed source area accounts for the tsunami waves reported in Omoa Bay. We show that the striking amplification observed in Omoa Bay is related to the trapping of waves due to the shallow submarine shelf surrounding the island.