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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 Poster presentation 1827<br />

Tsunami hazard estimation for the southern Kuril Island coast<br />

Dr. Victor Kaystrenko<br />

Russian Academy of sciences Institute of Marine Geology and Geophysics<br />

The Russian Far Eastern coast is a one of the most tectonically active margin of the Pacific area with<br />

frequent tsunami occurrence. After catastrophic tsunami in November 1952 that destroyed the most<br />

part of the Severo-Kurilsk town, up till now more than 40 tsunami were recorded on the Far East coast<br />

of our country, the height being more than 5 meters in 7 cases, and in 1952, 1963, 1969, 1994 the<br />

wave heights being up to 15 meters in some points. Tsunami hazard distribution along the Russian<br />

coast is not homogeneous and tsunamis are most frequent events on the Southern Kuril Island coast. It<br />

is known that a sequence of earthquakes exceeding an elected magnitude is really the Poissonian one<br />

and its main parameter is the recurrence functionF (h0) which is a mean frequency of tsunamis with<br />

height more then elected "threshold" h0. Analysis of the natural data showed that this function depends<br />

from two parameters: F(h0) = f exp ( -h0/H*). Parameter H* is calibrate (characteristic) tsunami height<br />

depended from the coastal point of tsunami observation, and f is the regional tsunami frequency, that<br />

varying very slowly along the Pacific coast and can be considered as a regional constant. Using the least<br />

square method these parameters have been calculated from the historical tsunami data set. Finally,<br />

characteristic tsunami heights H* were evaluated for 18 points on the Southern Kuril Island coast.<br />

Tsunami frequency for this region is f = 0.17 1/year and its standard deviation is σ(ln(f) = 0.13. These<br />

parameter allowed to estimate tsunami risk for this region. The work was supported by the grants of<br />

the Russian Foundation of Basic Research 05-05-64733 andFEB RAS I # 06-I-ON3-106.<br />

Keywords: tsunami, hazard, risk

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