The Sumatra tsunami of 26 December 2004 as observed in the North Pacific and North Atlantic oceans

The Mw=9.3 megathrust earthquake of December 26, 2004 off the coast of Sumatra in the Indian Ocean generated a catastrophic tsunami that caused widespread damage in coastal areas and left more than 226,000 people dead or missing. The Sumatra tsunami was accurately recorded by a large number of tide gauges throughout the world's oceans. This paper examines the amplitudes, frequencies and wave train structure of tsunami waves recorded by tide gauges located more than 20,000 km from the source area along the Pacific and Atlantic coasts of North America.

[1]  Maximum Entropy Spectral Analysis of Tsunamis along the Mexican Coast, 1957–1979 , 1980 .

[2]  The December 26th 2004 Tsunami Recorded along the Southeastern Coast of Brazil , 2007 .

[3]  P. Hattori,et al.  TSUNAMIS AND TSUNAMI-LIKE WAVES OF THE EASTERN UNITED STATES , 2002 .

[4]  J. Battjes Surf-Zone Dynamics , 1988 .

[5]  William J. Emery,et al.  Data Analysis Methods in Physical Oceanography , 1998 .

[6]  J. Tromp,et al.  The Great Sumatra-Andaman Earthquake , 2005 .

[7]  Vasily Titov,et al.  The Global Reach of the 26 December 2004 Sumatra Tsunami , 2005, Science.

[8]  K. Satake Tsunamis: Case Studies and Recent Developments , 2005 .

[9]  A. Rabinovich,et al.  Investigation of long waves in the tsunami frequency band on the southwestern shelf of Kamchatka , 1991 .

[10]  A. Rabinovich,et al.  Longwave Measurements for the Coast of British Columbia and Improvements to the Tsunami Warning Capability , 2004 .

[11]  K. Iida,et al.  Tsunamis: Their Science and Engineering , 1983 .

[12]  E. Kulikov,et al.  Dispersion of the Sumatra Tsunami waves in the Indian Ocean detected by satellite altimetry , 2006 .

[13]  B. Bornhold,et al.  The Grand Banks landslide-generated tsunami of November 18, 1929: preliminary analysis and numerical modeling , 2005 .

[14]  A. Roueff,et al.  Use of hydroacoustic and seismic arrays to observe rupture propagation and source extent of the Mw = 9.0 Sumatra earthquake , 2005 .

[15]  Emile A. Okal,et al.  Seismology: Speed and size of the Sumatra earthquake , 2005, Nature.

[16]  Ira Didenkulova,et al.  Analysis of Tide-Gauge Records of the 1883 Krakatau Tsunami , 2005 .

[17]  A. Dziewoński,et al.  Multiple CMT source analysis of the 2004 Sumatra earthquake , 2005 .

[18]  W. G. V. Dorn Some Tsunami Characteristics Deducible from Tide Records , 1984 .

[19]  B. Bornhold,et al.  The landslide tsunami of November 3, 1994, Skagway Harbor, Alaska , 1996 .

[20]  Thorkild Aarup,et al.  Tide gauge observations of the Indian Ocean tsunami, December 26, 2004 , 2005 .

[21]  F. González,et al.  Tsunami Dispersion Observed in the Deep Ocean , 1993 .

[22]  Kevin Horsburgh,et al.  Evidence for the Indonesian Tsunami in British tidal records , 2005 .

[23]  Tide gauge observations of the Indian ocean tsunami, December 26, 2004, in Buenos Aires coastal waters, Argentina , 2006 .

[24]  D. Huntley,et al.  INFRAGRAVITY WAVES IN STORM CONDITIONS , 1978 .

[25]  Efim Pelinovsky,et al.  Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption , 2003 .

[26]  Pedro M. A. Miranda,et al.  The 1755 Lisbon tsunami; evaluation of the tsunami parameters , 1998 .

[27]  NUMERICAL MODELING OF THE GLOBAL TSUNAMI , 2005 .

[28]  A. Dziewoński,et al.  A technique for the analysis of transient seismic signals , 1969 .

[29]  A. Rabinovich,et al.  Spectral analysis of tsunami waves: Separation of source and topography effects , 1997 .

[30]  Stefano Tinti,et al.  Tsunamis in the World , 1993 .

[31]  H. Kanamori,et al.  The Great Sumatra-Andaman Earthquake of 26 December 2004 , 2005, Science.

[32]  Sebastià Monserrat,et al.  Meteorological tsunamis near the Balearic and Kuril Islands: Descriptive and statistical analysis , 1996 .