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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS002 Oral Presentation 1748<br />

The 26 December 2004 Sumatra Tsunami in the Atlantic Ocean:<br />

Observations and Analysis<br />

Dr. Alexander Rabinovich<br />

Russian Academy of Sciences, Moscow, Russia Tsunami Laboratory, Institute of Oceanology<br />

<strong>IASPEI</strong><br />

Philip Woodworth, Richard Thomson<br />

The Mw = 9.3 megathrust earthquake of December 26, 2004 off the west coast of Sumatra in the<br />

Indian Ocean generated a widespread catastrophic tsunami. This was the first global tsunami to occur<br />

during the "instrumental era", and it was accurately recorded by a large number of tide gauges<br />

throughout the World Ocean, including many tide gauges in the Atlantic Ocean, at sites located ten to<br />

twenty five thousand kilometers from the source area. The Mid-Atlantic Ridge is shown to have served<br />

as a wave-guide for the 2004 event, efficiently transmitting tsunami energy from the source area to farfield<br />

regions of the Atlantic coasts of South and North America. Statistical characteristics (wave height,<br />

period, and arrival time) and spectral properties of the tsunami waves observed in the Atlantic are<br />

examined and summarized. This is the second part of a three-part study of the Working Group on Tide<br />

Gauge Measurements of the 2004 Sumatra Tsunami, IUGG Tsunami Commission. This first part focused<br />

on the Indian Ocean (PAGEOPH, 2007) while the third part will focus on the Pacific Ocean.<br />

Keywords: 2004, sumatra, atlantic

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