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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8314
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dc.contributor.authorallChini, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallPiscini, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallCinti, F. R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallAmici, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallNappi, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallDe Martini, P. M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2012-10-19T13:51:06Zen
dc.date.available2012-10-19T13:51:06Zen
dc.date.issued2013-03en
dc.identifier.urihttp://hdl.handle.net/2122/8314en
dc.description.abstractWe studied the disastrous effects of the tsunami triggered by the Mw 9.0 earthquake that occurred on 11 March 2011 offshore the Honshu island (Japan). The tsunami caused a huge amount of casualties and severe damage along most of the eastern coastline of the island. The dataset used is composed of images from ASTER (visible and thermal) and ENVISAT SAR sensors. The processing and the analysis of data from different sources were performed in order to obtain the tsunami inundation map of the Sendai coastal area, to analyze inland factors driving the tsunami inundation, and to detect the liquefaction effects in the Chiba bay area as well. The obtained inundation line, with a maximum value of about 6 km, has been jointly analyzed with DEM providing the run-up values, which are generally below 21 m in the ca. 60-km-long study area of Sendai. The analysis highlights that the coastal topography influences the inundation process: high-relief zones record the lowest inundation distances, while within the plain the waves entered inland for at least 4 km. We did not observe significant direct effects of the vegetation cover on the inland water penetration along the whole investigated area, nor of the different orientation of the coastline. Moreover, from SAR coherence and intensity correlation a wide area of subsidence is mapped at Chiba bay, which is reasonably related to strong ground shaking and pervasive liquefaction.en
dc.language.isoEnglishen
dc.publisher.nameIEEE / Institute of Electrical and Electronics Engineers Incorporateden
dc.relation.ispartofIEEE geoscience and remote sensing letters : a publication of the IEEE Geoscience and Remote Sensing Societyen
dc.relation.ispartofseries2/10 (2013)en
dc.subject2011 Japan tsunamien
dc.subjectwave inundationen
dc.subjectliquefactionen
dc.subjectSAR, Optical and Thermal dataen
dc.titleThe 2011 Tohoku-Oki (Japan) tsunami inundation and liquefaction investigated through optical, thermal and SAR dataen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber347-351en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoringen
dc.identifier.doi10.1109/LGRS.2012.2205661en
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[9] F. Bovolo, and L. Bruzzone, “A Split-Based Approach to Unsupervised Change Detection in Large-Size Multitemporal Images: Application to Tsunami-Damage Assessment,” IEEE Trans. Geosci. Remote Sens., vol. 45, no. 6, pp. 1658.1670, 2007. [10] M. Chini, C. Bignami, S. Stramondo and N. Pierdicca, “Uplift and subsidence due to the 26 December 2004 Indonesian earthquake detected by SAR data,” Int. J. Remote Sens., vol. 29, no. 13, pp. 3891– 3910, 2008. [11] C. C. Liu, J. G. Liu, C. W. Lin, A. M. Wu, S. H. Liu, and C. L. Shieh, “Image processing of FORMOSAT‐2 data for monitoring the South Asia tsunami,” Int. J. Remote Sens., vol. 28, no. 13–14, pp. 3093–3111, 2007. [12] A. S. Belward, H. J. Stibig, H. Eva, F. Rembold, T. Bucha, A. Hartley, R. Beuchle, D. Khudhairy, M. Michielon, and D. Mollicone, “Mapping severe damage to land cover following the 2004 Indian Ocean tsunami using moderate spatial resolution satellite imagery,” Int. J. Remote Sens., vol. 28, no. 13–14, pp. 2977–2994, 2007. 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Kapourani, “Critical Factors for Run-up and Impact of the Tohoku Earthquake Tsunami,” International Journal of Geosciences, vol. 2, pp. 310-317, 2011. [30] N. Mori, T. Takahashi, T. Yasuda, and H. Yanagisawa, “Survey of 2011 Tohoku earthquake tsunami inundation and run-up,” Geophysical Research Letters, vol. 38, L00G14, 2011. [31] T. Kishida, “Phase 1: Liquefaction Damages on Reclamation Lands In Chiba Bay Area After Tohoku Pacific Coast Earthquake On March 11, 2011,” freesia.arch.ues.tmu.ac.jp/TohokuEQ2011/201103/msg48.1.pdf. [32] H. A. Zebker, and J. Villasenor, “Decorrelation in interferometric radar echoes,” IEEE Trans. Geosci. Remote Sens., vol. 30, no. 5, pp. 950–959, 1992.en
dc.description.obiettivoSpecifico1.10. TTC - Telerilevamentoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn1545-598Xen
dc.relation.eissn1558-0571en
dc.contributor.authorChini, M.en
dc.contributor.authorPiscini, A.en
dc.contributor.authorCinti, F. R.en
dc.contributor.authorAmici, S.en
dc.contributor.authorNappi, R.en
dc.contributor.authorDe Martini, P. M.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptLuxembourg Institute of Science and Technology (LIST)-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0001-5545-3611-
crisitem.author.orcid0000-0003-1068-3223-
crisitem.author.orcid0000-0003-2410-646X-
crisitem.author.orcid0000-0002-1552-4398-
crisitem.author.orcid0000-0002-3598-5191-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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