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Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/19556
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dc.contributor.authorMuhari, A-
dc.contributor.authorHeidarzadeh, M-
dc.contributor.authorSusmoro, H-
dc.contributor.authorNugroho, HD-
dc.contributor.authorKriswati, E-
dc.contributor.authorSupartoyo-
dc.contributor.authorWijanarto, AB-
dc.contributor.authorImamura, F-
dc.contributor.authorArikawa, T-
dc.date.accessioned2019-11-12T11:29:41Z-
dc.date.available2019-11-12T11:29:41Z-
dc.date.issued2019-11-21-
dc.identifier.citationMuhari, A., Heidarzadeh, M., Susmoro, H., Nugroho, H.D., Kriswati, E., Supartoyo, Wijanarto, A.B., Imamura, F. and Arikawa, T . (2019) 'The December 2018 Anak Krakatau Volcano Tsunami as Inferred from Post-Tsunami Field Surveys and Spectral Analysis', Pure and Applied Geophysics, 2019, 176 (12), pp. 5219 - 5233. doi: 10.1007/s00024-019-02358-2.en_US
dc.identifier.issn0033-4553-
dc.identifier.urihttps://bura.brunel.ac.uk/handle/2438/19556-
dc.description.abstractCopyright © The Author(s) 2019. We present analysis of the December 2018 Anak Krakatau tsunami in Sunda Strait, Indonesia, from a combination of post-tsunami field surveys, bathymetric changes and spectral analysis of the tsunami tide gauge records. Post-tsunami surveys revealed moderate tsunami height along the coast of Sumatra and Java with maximum surveyed runup of 13.5 m and maximum inundation distance of 330 m. At small islands located close to the volcano, extreme tsunami impacts were observed indicating not only a huge tsunami was generated by large amounts of collapse material which caused notable changes of seafloor bathymetry, but also indicates the role of those small islands in reducing tsunami height that propagated to the mainland of Indonesia. Our spectral analysis of tide gauge records showed that the tsunami’s dominant period was 6.6–7.4 min, indicating the short-period nature of the 2018 Sunda Strait tsunami.-
dc.description.sponsorshipInternational Research Institute of Disaster Science, Tohoku University, Japan; Royal Society (grant number CHL\R1\180173); Brunel University London (Brunel Research Initiative and Enterprise Fund 2017/18, BUL BRIEF).en_US
dc.format.extent5219 - 5233-
dc.format.mediumPrint-Electronic-
dc.language.isoenen_US
dc.publisherSpringer International Publishingen_US
dc.rightsOpen Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.-
dc.rightsCopyright © The Author(s) 2019. Rights and permissions Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.-
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/-
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/-
dc.subjectSunda Strait tsunamien_US
dc.subjectAnak Krakatau volcanoen_US
dc.subjectpost-tsunami surveyen_US
dc.titleThe December 2018 Anak Krakatau Volcano Tsunami as Inferred from Post-Tsunami Field Surveys and Spectral Analysisen_US
dc.typeArticleen_US
dc.identifier.doihttps://doi.org/10.1007/s00024-019-02358-2-
dc.relation.isPartOfPure and Applied Geophysics-
pubs.issue12-
pubs.publication-statusPublished-
pubs.volume176-
dc.identifier.eissn1420-9136-
Appears in Collections:Dept of Mechanical and Aerospace Engineering Research Papers

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