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A macroseismic model of a tsunami source and estimation of its efficiency by numerical modeling. / Poplavskii, A. A.; Zolotukhin, D. E.; Khramushin, V. N.

In: Journal of Volcanology and Seismology, Vol. 6, No. 1, 01.02.2012, p. 58-64.

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Harvard

Poplavskii, AA, Zolotukhin, DE & Khramushin, VN 2012, 'A macroseismic model of a tsunami source and estimation of its efficiency by numerical modeling', Journal of Volcanology and Seismology, vol. 6, no. 1, pp. 58-64. https://doi.org/10.1134/S0742046311060066

APA

Vancouver

Author

Poplavskii, A. A. ; Zolotukhin, D. E. ; Khramushin, V. N. / A macroseismic model of a tsunami source and estimation of its efficiency by numerical modeling. In: Journal of Volcanology and Seismology. 2012 ; Vol. 6, No. 1. pp. 58-64.

BibTeX

@article{176db68a04f04051a20cf2bf1d0ca758,
title = "A macroseismic model of a tsunami source and estimation of its efficiency by numerical modeling",
abstract = "A typical model of the source of a tsunami ({"}macroseismic source{"}) is suggested for use in approximate estimation of maximum tsunami height using straightforward numerical modeling. In this paper the model is tested using three actual events: the 1952 North Kuril Is., 1971 Moneron, and 1994 Shikotan earthquakes, which excited considerable tsunamis at Russia's Far East coasts. Comparison of the maximum tsunami runup values as obtained in numerical experiments with observations of actual tsunamis showed that the numerical model proposed here is suitable for crude estimation of tsunami runup and tsunami waiting times for coastal population centers in the near zone of a tsunami source.",
author = "Poplavskii, {A. A.} and Zolotukhin, {D. E.} and Khramushin, {V. N.}",
year = "2012",
month = feb,
day = "1",
doi = "10.1134/S0742046311060066",
language = "English",
volume = "6",
pages = "58--64",
journal = "Journal of Volcanology and Seismology",
issn = "0742-0463",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - A macroseismic model of a tsunami source and estimation of its efficiency by numerical modeling

AU - Poplavskii, A. A.

AU - Zolotukhin, D. E.

AU - Khramushin, V. N.

PY - 2012/2/1

Y1 - 2012/2/1

N2 - A typical model of the source of a tsunami ("macroseismic source") is suggested for use in approximate estimation of maximum tsunami height using straightforward numerical modeling. In this paper the model is tested using three actual events: the 1952 North Kuril Is., 1971 Moneron, and 1994 Shikotan earthquakes, which excited considerable tsunamis at Russia's Far East coasts. Comparison of the maximum tsunami runup values as obtained in numerical experiments with observations of actual tsunamis showed that the numerical model proposed here is suitable for crude estimation of tsunami runup and tsunami waiting times for coastal population centers in the near zone of a tsunami source.

AB - A typical model of the source of a tsunami ("macroseismic source") is suggested for use in approximate estimation of maximum tsunami height using straightforward numerical modeling. In this paper the model is tested using three actual events: the 1952 North Kuril Is., 1971 Moneron, and 1994 Shikotan earthquakes, which excited considerable tsunamis at Russia's Far East coasts. Comparison of the maximum tsunami runup values as obtained in numerical experiments with observations of actual tsunamis showed that the numerical model proposed here is suitable for crude estimation of tsunami runup and tsunami waiting times for coastal population centers in the near zone of a tsunami source.

UR - http://www.scopus.com/inward/record.url?scp=84857851693&partnerID=8YFLogxK

U2 - 10.1134/S0742046311060066

DO - 10.1134/S0742046311060066

M3 - Article

AN - SCOPUS:84857851693

VL - 6

SP - 58

EP - 64

JO - Journal of Volcanology and Seismology

JF - Journal of Volcanology and Seismology

SN - 0742-0463

IS - 1

ER -

ID: 45862540