Near-field propagation of tsunamis from megathrust earthquakes

We investigate controls on tsunami generation and propagation in the near-field of great megathrust earthquakes using a series of numerical simulations of subduction and tsunamigenesis on the Sumatran forearc. The Sunda megathrust here is a...

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Main Authors: McCloskey, John, Antonioli, Andrea, Piatanesi, Alessio, Sieh, Kerry, Steacy, Sandy, Cocco, Massimo, Giunchi, Carlo, Huang, Jian Dong, Dunlop, Paul, Nalbant, Suleyman S.
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Language:English
Published: 2012
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Online Access:https://hdl.handle.net/10356/95545
http://hdl.handle.net/10220/8658
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-955452020-09-26T21:24:29Z Near-field propagation of tsunamis from megathrust earthquakes McCloskey, John Antonioli, Andrea Piatanesi, Alessio Sieh, Kerry Steacy, Sandy Cocco, Massimo Giunchi, Carlo Huang, Jian Dong Dunlop, Paul Nalbant, Suleyman S. DRNTU::Science::Geology::Volcanoes and earthquakes We investigate controls on tsunami generation and propagation in the near-field of great megathrust earthquakes using a series of numerical simulations of subduction and tsunamigenesis on the Sumatran forearc. The Sunda megathrust here is advanced in its seismic cycle and may be ready for another great earthquake. We calculate the seafloor displacements and tsunami wave heights for about 100 complex earthquake ruptures whose synthesis was informed by reference to geodetic and stress accumulation studies. Remarkably, results show that, for any near-field location: (1) the timing of tsunami inundation is independent of slipdistribution on the earthquake or even of its magnitude, and (2) the maximum wave height is directly proportional to the vertical coseismic displacement experienced at that location. Both observations are explained by the dominance of long wavelength crustal flexure in near-field tsunamigenesis. The results show, for the first time, that a single estimate of vertical coseismic displacement might provide a reliable short-term forecast of the maximum height of tsunami waves. Published version 2012-09-27T07:12:26Z 2019-12-06T19:16:59Z 2012-09-27T07:12:26Z 2019-12-06T19:16:59Z 2007 2007 Journal Article McCloskey, J., Antonioli, A., Piatanesi, A., Sieh, K., Steacy, S., Nalbant, S. S., et al. (2007). Near-field propagation of tsunamis from megathrust earthquakes. Geophysical Research Letters, 34(14). 0094-8276 https://hdl.handle.net/10356/95545 http://hdl.handle.net/10220/8658 10.1029/2007GL030494 en Geophysical research letters © 2007 the American Geophysical Union. This paper was published in Geophysical Research Letters and is made available as an electronic reprint (preprint) with permission of the American Geophysical Union. The paper can be found at the following official DOI: http://dx.doi.org/10.1029/2007GL030494. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law. application/pdf
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic DRNTU::Science::Geology::Volcanoes and earthquakes
spellingShingle DRNTU::Science::Geology::Volcanoes and earthquakes
McCloskey, John
Antonioli, Andrea
Piatanesi, Alessio
Sieh, Kerry
Steacy, Sandy
Cocco, Massimo
Giunchi, Carlo
Huang, Jian Dong
Dunlop, Paul
Nalbant, Suleyman S.
Near-field propagation of tsunamis from megathrust earthquakes
description We investigate controls on tsunami generation and propagation in the near-field of great megathrust earthquakes using a series of numerical simulations of subduction and tsunamigenesis on the Sumatran forearc. The Sunda megathrust here is advanced in its seismic cycle and may be ready for another great earthquake. We calculate the seafloor displacements and tsunami wave heights for about 100 complex earthquake ruptures whose synthesis was informed by reference to geodetic and stress accumulation studies. Remarkably, results show that, for any near-field location: (1) the timing of tsunami inundation is independent of slipdistribution on the earthquake or even of its magnitude, and (2) the maximum wave height is directly proportional to the vertical coseismic displacement experienced at that location. Both observations are explained by the dominance of long wavelength crustal flexure in near-field tsunamigenesis. The results show, for the first time, that a single estimate of vertical coseismic displacement might provide a reliable short-term forecast of the maximum height of tsunami waves.
format Article
author McCloskey, John
Antonioli, Andrea
Piatanesi, Alessio
Sieh, Kerry
Steacy, Sandy
Cocco, Massimo
Giunchi, Carlo
Huang, Jian Dong
Dunlop, Paul
Nalbant, Suleyman S.
author_facet McCloskey, John
Antonioli, Andrea
Piatanesi, Alessio
Sieh, Kerry
Steacy, Sandy
Cocco, Massimo
Giunchi, Carlo
Huang, Jian Dong
Dunlop, Paul
Nalbant, Suleyman S.
author_sort McCloskey, John
title Near-field propagation of tsunamis from megathrust earthquakes
title_short Near-field propagation of tsunamis from megathrust earthquakes
title_full Near-field propagation of tsunamis from megathrust earthquakes
title_fullStr Near-field propagation of tsunamis from megathrust earthquakes
title_full_unstemmed Near-field propagation of tsunamis from megathrust earthquakes
title_sort near-field propagation of tsunamis from megathrust earthquakes
publishDate 2012
url https://hdl.handle.net/10356/95545
http://hdl.handle.net/10220/8658
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