2008
DOI: 10.1007/s00024-008-0414-9
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Numerical Modeling and Observations of Tsunami Waves in Alberni Inlet and Barkley Sound, British Columbia

Abstract: Alberni Inlet is a long and narrow fjord adjacent to Barkley Sound on the Pacific Coast of Vancouver Island, Canada. Port Alberni, at the head of the inlet, was affected in 1964 by the largest Pacific tsunami waves in Canadian history. We use observations and results from two numerical models to investigate the resonant characteristics of the region and amplification of tsunami waves in Barkley Sound and Alberni Inlet. The first model (A) was forced at its open boundary with a stationary autoregressive signal,… Show more

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Cited by 24 publications
(8 citation statements)
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“…Wave resonance has been observed in Port Alberni, located at the head of a narrow inlet in the west past of Vancouver island, during the 1964 Alaskan earthquake (Fine et al, 2008). The recorded wave heights in the port were 3-4 times larger than in the adjacent areas, often recorded in the third or later waves, and the tsunami oscillations continued for days after the event (Fine et al, 2008). It is likely that local topographic features can contribute to tsunami amplification also in other parts of the region.…”
Section: Predictions With Two Families Of Scenariosmentioning
confidence: 99%
“…Wave resonance has been observed in Port Alberni, located at the head of a narrow inlet in the west past of Vancouver island, during the 1964 Alaskan earthquake (Fine et al, 2008). The recorded wave heights in the port were 3-4 times larger than in the adjacent areas, often recorded in the third or later waves, and the tsunami oscillations continued for days after the event (Fine et al, 2008). It is likely that local topographic features can contribute to tsunami amplification also in other parts of the region.…”
Section: Predictions With Two Families Of Scenariosmentioning
confidence: 99%
“…One of the regions on Vancouver Island to receive the most significant tsunami damage was the town of Port Alberni, tied to an inlet on the west side of the island. Several hours after the Great Alaskan Earthquake struck, multiple waves flowed up the Alberni Inlet, cresting at 8 m and striking the Port Alberni region, washing away 55 homes and damaging nearly 400 others (37). Kidd et al (16) sampled the Port Alberni region, which is approximately 40 km from the eastern edge of the island, finding C.…”
Section: The Great Alaskan Earthquake and Tsunamismentioning
confidence: 99%
“…coast was at Port Alberni on March 28, 1964 (WIGEN andWHITE, 1964;FINE et al, 2008) and that station was in continuous operation from 1970 to 1997, however, lulled by a long period of little tsunami activity and faced with budget restrictions the station was then shut down. It was only as a result of the review of analogue records (1981)(1982)(1983)(1984)(1985)(1986)(1987)(1988)(1989)(1990)(1991)(1992)(1993)(1994)(1995)(1996)(1997) that the importance of Port Alberni for tsunami research was again appreciated.…”
Section: Observational Problemsmentioning
confidence: 99%
“…Changing the data recording to 6-min sample intervals would reduce the data storage and data transmission costs, however, the Nyquist period in that case would become 12 min. The major topographic admittance peaks at most of the stations were determined to be located at periods less than 12 min (cf., RABINOVICH and STEPHENSON, 2004;FINE et al, 2008). Also some of the recent tsunami events (2001 Queen Charlotte;2004 Vancouver Island;2005 California;2007 Kuril Islands) had major source energy at relatively high frequencies (cf., RABINOVICH and STEPHENSON, 2004;RABINOVICH et al, 2006bRABINOVICH et al, , 2008b.…”
Section: Observational Problemsmentioning
confidence: 99%