A Probabilistic Tsunami Hazard Assessment for Western Australia

The occurrence of the Indian Ocean Tsunami on 26 December, 2004 has raised concern about the difficulty in determining appropriate tsunami mitigation measures in Australia, due to the lack of information on the tsunami threat. A first step in the development of such measures is a tsunami hazard assessment, which gives an indication of which areas of coastline are most likely to experience tsunamis, and how likely such events are. Here we present the results of a probabilistic tsunami hazard assessment for Western Australia (WA). Compared to other parts of Australia, the WA coastline experiences a relatively high frequency of tsunami occurrence. This hazard is due to earthquakes along the Sunda Arc, south of Indonesia. Our work shows that large earthquakes offshore of Java and Sumba are likely to be a greater threat to WA than those offshore of Sumatra or elsewhere in Indonesia. A magnitude 9 earthquake offshore of the Indonesian islands of Java or Sumba has the potential to significantly impact a large part of the West Australian coastline. The level of hazard varies along the coast, but is highest along the coast from Carnarvon to Dampier. Tsunamis generated by other sources (e.g., large intra-plate events, volcanoes, landslides and asteroids) were not considered in this study.

[1]  J. Nott,et al.  Extreme Marine Inundations (Tsunamis?) of Coastal Western Australia , 2003, The Journal of Geology.

[2]  C. Cornell Engineering seismic risk analysis , 1968 .

[3]  D. Burbidge,et al.  Historic records of teletsunami in the Indian Ocean and insights from numerical modelling , 2007 .

[4]  E. Asphaug,et al.  Asteroid Impact Tsunami: A Probabilistic Hazard Assessment , 2000 .

[5]  Yoshinori Shigihara,et al.  Wave Dispersion Study in the Indian Ocean-Tsunami of December 26, 2004 , 2006 .

[6]  T. Rikitake,et al.  Tsunami hazard probability in Japan , 1988 .

[7]  L. Ruff Do trench sediments affect great earthquake occurrence in subduction zones? , 1989 .

[8]  Javier F. Pacheco,et al.  Nature of seismic coupling along simple plate boundaries of the subduction type , 1993 .

[9]  David Burbidge,et al.  Assessing the threat to Western Australia from tsunami generated by earthquakes along the Sunda Arc , 2007 .

[10]  J. Braun,et al.  Analogue models of obliquely convergent continental plate boundaries , 1998 .

[11]  S. Kramer Geotechnical Earthquake Engineering , 1996 .

[12]  D. Douglas,et al.  Variations in the Arctic's multiyear sea ice cover: A neural network analysis of SMMR‐SSM/I data, 1979–2004 , 2005 .

[13]  Hai Cheng,et al.  Source parameters of the great Sumatran megathrust earthquakes of 1797 and 1833 inferred from coral microatolls , 2006 .

[14]  P. Bland,et al.  Efficient disruption of small asteroids by Earth's atmosphere , 2003, Nature.

[15]  Rongjiang Wang,et al.  Erratum to: "Computation of deformation induced by earthquakes in a multi-layered elastic crust - FORTRAN programs EDGRN/EDCMP": [Computers & Geosciences, 29(2) (2003) 195-207] , 2006, Comput. Geosci..

[16]  Nearshore Flow Velocity of Southwest Hokkaido Earthquake Tsunami , 2000 .

[17]  Yehuda Bock,et al.  Crustal motion in Indonesia from Global Positioning System measurements , 2003 .

[18]  Dominique Reymond,et al.  The mechanism of great Banda Sea earthquake of 1 February 1938: applying the method of preliminary determination of focal mechanism to a historical event , 2003 .

[19]  S. Acharyya Break-up of the Greater Indo-Australian Continent and accretion of blocks framing South and East Asia , 1998 .

[20]  W. Mccann,et al.  Seismic history and seismotectonics of the Sunda Arc , 1987 .

[21]  H. Melosh Impact-generated Tsunamis: An Over-rated Hazard , 2003 .

[22]  C. Scholz The Mechanics of Earthquakes and Faulting , 1990 .

[23]  Tom Parsons,et al.  Probabilistic Analysis of Tsunami Hazards* , 2006 .

[24]  Hiroo Kanamori,et al.  Seismicity and the subduction process , 1980 .

[25]  Michael Antolik,et al.  The June 2000 Mw 7.9 earthquakes south of Sumatra: Deformation in the India–Australia Plate , 2003 .

[26]  Steven R. Chesley,et al.  A Quantitative Assessment of the Human and Economic Hazard from Impact-generated Tsunami , 2006 .

[27]  Stuart P. Nishenko,et al.  Circum-Pacific seismic potential: 1989–1999 , 1991 .

[28]  R. Mccaffrey Active tectonics of the Eastern Sunda and Banda Arcs , 1988 .

[29]  P. Bird An updated digital model of plate boundaries , 2003 .

[30]  Paul Somerville,et al.  PROBABILISTIC ANALYSIS OF STRONG GROUND MOTION AND TSUNAMI HAZARDS IN SOUTHEAST ASIA , 2007 .

[31]  S. Stein,et al.  Ultralong Period Seismic Study of the December 2004 Indian Ocean Earthquake and Implications for Regional Tectonics and the Subduction Process , 2007 .

[32]  S. Harmsen,et al.  Geographic Deaggregation of Seismic Hazard in the United States , 2001 .

[33]  E. Carminati,et al.  Slab dip vs. lithosphere age: No direct function , 2005 .

[34]  Y. Kagan,et al.  Plate-Tectonic Analysis of Shallow Seismicity: Apparent Boundary Width, Beta, Corner Magnitude, Coupled Lithosphere Thickness, and Coupling in Seven Tectonic Settings , 2004 .

[35]  S. Day,et al.  Cumbre Vieja Volcano—Potential collapse and tsunami at La Palma, Canary Islands , 2001 .

[36]  Phil R. Cummins,et al.  The potential for giant tsunamigenic earthquakes in the northern Bay of Bengal , 2007, Nature.

[37]  P. Lynett,et al.  Offshore breaking of impact tsunami: The Van Dorn effect revisited , 2005 .

[38]  J. Keene,et al.  Submarine slope failures of the southeast Australian continental slope: a thinly sedimented margin , 1992 .

[39]  Eric L. Geist,et al.  Complex earthquake rupture and local tsunamis , 2002 .

[40]  R. Blakely,et al.  Basin‐centered asperities in great subduction zone earthquakes: A link between slip, subsidence, and subduction erosion? , 2003 .

[41]  H. Berckhemer,et al.  A magnitude scale for very large earthquakes , 1978 .

[42]  Kelin Wang,et al.  The updip and downdip limits to great subduction earthquakes: Thermal and structural models of Casca , 1999 .

[43]  Robin K. McGuire,et al.  FORTRAN computer program for seismic risk analysis , 1976 .

[44]  Kelin Wang,et al.  Thermal constraints on the zone of major thrust earthquake failure: The Cascadia Subduction Zone , 1993 .

[45]  N. Chamot-Rooke,et al.  Intraplate shortening in the central Indian Ocean determined from a 2100-km-long north-south deep seismic reflection profile , 1993 .

[46]  David A. Yuen,et al.  Tsunami hazards along Chinese coast from potential earthquakes in South China Sea , 2007 .

[47]  R. Lawrence Edwards,et al.  Submergence and uplift associated with the giant 1833 Sumatran subduction earthquake: Evidence from coral microatolls , 1999 .

[48]  H. Kopp BSR occurrence along the Sunda margin: evidence from seismic data , 2002 .

[49]  Javier F. Pacheco,et al.  Seismic moment catalog of large shallow earthquakes, 1900 to 1989 , 1992, Bulletin of the Seismological Society of America.

[50]  W. Spence The 1977 Sumba earthquake series: Evidence for Slab pull force acting at a subduction zone , 1986 .

[51]  Yan Y. Kagan,et al.  Seismic moment distribution revisited: II. Moment conservation principle , 2002 .

[52]  R. Perry,et al.  Persistent cytoplasmic synthesis of ribosomal proteins during the selective inhibition of ribosomal RNA synthesis. , 1971, Nature: New biology.