HR: 1340h
AN: S53A-1015    [Abstracts]
TI: Hazard from far-field tsunami at Hilo: Earthquakes from the Ring of Fire
AU: Arcas, D
EM: Diego.Arcas@noaa.gov
AF: NOAA Center for Tsunami Research PMEL/University of Washington, 7600 Sand Point Way NE, Seattle, WA 98115, United States
AU: * Weiss, R
EM: Robert.Weiss@noaa.gov
AF: NOAA Center for Tsunami Research PMEL/University of Washington, 7600 Sand Point Way NE, Seattle, WA 98115, United States
AU: Titov, V
AF: NOAA Center for Tsunami Research PMEL/University of Washington, 7600 Sand Point Way NE, Seattle, WA 98115, United States
AB: Historical data and modeling are used to study tsunami hazard at Hilo, Hawaii. Hilo has one of the best historical tsunami record in the US. Considering the tsunami observations from the early eighteen hundreds until today reveals that the number of observed events per decade depends on the awareness of tsunami events. The awareness appears to be a function of the observation techniques such as seismometers and communication devices, as well as direct measurements. Three time periods can be identified, in which the number of observed events increases from one event per decade in the first period to 7.7 in the second, to 9.4 events per decade in the third one. A total of 89 events from far-field sources have been encountered. In contrast only 11 events have been observed with sources in the near field. To remove this historical observation bias from the hazard estimate, we have complimented the historical analysis with a modeling study. We have carried out modeling of 1476 individual earthquakes along the subduction zones of the Pacific Ocean in four different magnitude levels (7.5, 8.2, 8.7 and 9.3). The maximum run up and maximum peak at the tide gauge is plotted for the different magnitude levels to reveal sensitive and source areas of tsunami waves for Hilo and a linear scaling of both parameters for small, but non-linear scaling for larger earthquakes
DE: 0545 Modeling (4255)
SC: Seismology [S]
MN: 2007 Fall Meeting