Probabilistic Tsunami Hazard Assessment (PTHA) for Crescent City, CA

[1]  C. Amante,et al.  ETOPO1 arc-minute global relief model : procedures, data sources and analysis , 2009 .

[2]  K. Satake,et al.  Asperity Distribution of the 1952 Great Kamchatka Earthquake and its Relation to Future Earthquake Potential in Kamchatka , 1999 .

[3]  P. Silver,et al.  Elevation changes and the Great 1960 Chilean Earthquake: Support for aseismic slip , 1989 .

[4]  J. Borrero,et al.  Observations and Impacts from the 2010 Chilean and 2011 Japanese Tsunamis in California (USA) , 2013, Pure and Applied Geophysics.

[5]  P. Silver,et al.  Low‐frequency source characteristics of the great 1960 Chilean earthquake , 1989 .

[6]  R. LeVeque,et al.  HIGH-RESOLUTION FINITE VOLUME METHODS FOR THE SHALLOW WATER EQUATIONS WITH BATHYMETRY AND DRY STATES , 2008 .

[7]  K. Satake,et al.  Unusually large earthquakes inferred from tsunami deposits along the Kuril trench , 2003, Nature.

[8]  R. LeVeque.  Finite Volume Methods for Hyperbolic Problems: Characteristics and Riemann Problems for Linear Hyperbolic Equations , 2002 .

[9]  Steven N. Ward,et al.  The 1960 Chile earthquake: inversion for slip distribution from surface deformation , 1990 .

[10]  Chen Ji,et al.  Focal mechanism and slip history of the 2011 Mw 9.1 off the Pacific coast of Tohoku Earthquake, constrained with teleseismic body and surface waves , 2011 .

[11]  Numerical Simulations of the 1960 Chilean Tsunami Propagation and Inundation at Hilo, Hawaii , 1995 .

[12]  H. Kanamori,et al.  The rupture process and asperity distribution of three great earthquakes from long-period diffracted P-waves , 1983 .

[13]  O. A. Braitseva,et al.  A millennial-scale record of Holocene tsunamis on the Kronotskiy Bay coast, Kamchatka, Russia , 2003, Quaternary Research.

[14]  Randall J. LeVeque,et al.  The GeoClaw software for depth-averaged flows with adaptive refinement , 2010, 1008.0455.

[15]  I. Cifuentes.  The 1960 Chilean earthquakes , 1989 .

[16]  S. Ward.  Earthquake mechanisms and tsunami generation: The Kurile Islands event of 13 October 1963 , 1982 .

[17]  F. Waldhauser,et al.  Juan de Fuca slab geometry and its relation to Wadati-Benioff zone seismicity , 2012 .

[18]  Mark D. Petersen,et al.  Simulations of Seismic Hazard for the Pacific Northwest of the United States from Earthquakes Associated with the Cascadia Subduction Zone , 2002 .

[19]  Randall J. LeVeque,et al.  Comparison of Earthquake Source Models for the 2011 Tohoku Event Using Tsunami Simulations and Near‐Field Observations , 2013 .

[20]  F. Waldhauser,et al.  A Geo-referenced 3D model of the Juan de Fuca Slab and associated seismicity , 2011 .

[21]  Jeffrey R. Johnson,et al.  Probabilistic Tsunami Hazard Assessment at Seaside, Oregon, for Near- and Far-Field Seismic Sources , 2009 .

[22]  Harold O. Mofjeld,et al.  Effects of Tides on Maximum Tsunami Wave Heights: Probability Distributions* , 2007 .

[23]  G. Beroza,et al.  A spatial random field model to characterize complexity in earthquake slip , 2002 .

[24]  Randall J. LeVeque,et al.  Tsunami modelling with adaptively refined finite volume methods* , 2011, Acta Numerica.

[25]  Vasily Titov,et al.  Implementation and testing of the Method of Splitting Tsunami (MOST) model , 1997 .

[26]  David L. George,et al.  Finite volume methods and adaptive refinement for tsunami propagation and inundation , 2006 .

[27]  F. Pollitz,et al.  Viscoelastic‐cycle model of interseismic deformation in the northwestern United States , 2010 .

[28]  K. Abe.  Size of great earthquakes of 1837–1974 inferred from tsunami data , 1979 .