Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5644
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dc.contributor.authorallVucetic, T.; Obala 4, Vela Luka, Croatiaen
dc.contributor.authorallVilibic, I.; Institute of Oceanography and Fisheries, Split, Croatiaen
dc.contributor.authorallTinti, S.; Dip.to di Fisica, Settore Geofisica, University of Bolognaen
dc.contributor.authorallMaramai, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.date.accessioned2010-01-18T10:40:34Zen
dc.date.available2010-01-18T10:40:34Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5644en
dc.description.abstractThis paper describes an extraordinary tsunami-like event that occurred on 21 June 1978 that encompassed the middle and south Adriatic Sea. The flood had its culmination in Vela Luka, where a maximum wave height of 6 m was reported. This paper contains a detailed description of the event as seen by eyewitnesses, its outreach along both the eastern and western coasts, and the aftermath and recovery activities in Vela Luka. All available records have been collected and analysed to detect the source and the generating mechanism of the long ocean waves. Seismic generation is fully excluded from the consideration, while a submarine landslide seems rather unrealistic as it does not explain the characteristics of the measured ocean waves. Therefore, the source of the event was presumably in the atmosphere, where a travelling disturbance was detected that had the capability to resonantly transfer energy to the ocean via the Proudman resonance mechanism. Although these data prove the proposed mechanism, the final confirmation for such a scenario should come from a process-oriented numerical modelling study.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofPhysics and Chemistry of the Earthen
dc.relation.ispartofseries/34 (2009)en
dc.subjectmeteotsunamien
dc.subjectcoastal flooden
dc.subjectAdriatic seaen
dc.subjectAtmospheric wavesen
dc.titleThe great Adriatic flood of 21 June 1978 revisited: an overview of the reportsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber894-903en
dc.subject.INGV05. General::05.02. Data dissemination::05.02.04. Hydrogeological dataen
dc.identifier.doi10.1016/j.pce.2009.08.005en
dc.relation.referencesReferences Bedosti, B., 1980. Considerazioni sul maremoto adriatico (tsunami) del 21.6.1978. Supplemento Bollettini Sismici Provv., 12-14-20. pp. 2–17 (in Italian). Herak, M., Orlic´ , M., Kunovec-Varga, M., 2001. Did the Makarska earthquake of 1962 generate a tsunami in the central Adriatic archipelago? Journal of Geodynamics 31, 71–86. Hodzˇic´ , M., 1979/1980. Occurrences of exceptional sea-level oscillations in the Vela Luka Bay (in Croatian). Priroda 68, 52–53. Hodzˇic´ , 1986. Long Gravity Waves Generated by Cyclones and Free Bay Oscillations (seiches) in the Adriatic. PhD Thesis, Faculty of Science, University of Belgrade, 128 pp (in Croatian). ICG-NEAMTWS, 2008. Tsunami Early Warning and Mitigation System in the North Eastern Atlantic, the Mediterranean and Connected Seas, NEAMTWS, Implementation Plan. IOC Technical Series No. 73. UNESCO. 46 pp. Lindzen, R.S., Tung, K.-K., 1976. Banded convective activity and ducted gravity waves. Monthly Weather Review 104, 1602–1617. Maramai, A., Graziani, L., Tinti, S., 2007. Investigation on tsunami effects in the central Adriatic Sea during the last century – a contribution. Natural Hazards and Earth System Sciences 7, 15–19. Minisini, D., Trincardi, F., Asioli, A., 2006. Evidence of slope instability in the Southwestern Adriatic Margin. Natural Hazards and Earth System Sciences 6, 1– 20. Orlic´ , M., 1980. About a possible occurrence of the Proudman resonance in the Adriatic. Thalassia Jugoslavica 16, 79–88. Orlic´ , M., 1983/1984. Are there tsunamis in the Adriatic? (in Croatian). Priroda 72, 310–311. Paulatto, M., Pinat, T., Romanelli, F., 2007. Tsunami hazard scenarios in the Adriatic Sea domain. Natural Hazards and Earth System Sciences 7, 309–325. Proudman, J., 1929. The effects on the sea of changes in atmospheric pressure. Geophysical Supplement to Monthly Notices of the Royal Astronomical Society 2, 197–209. Šepic´ , J., Vilibic´ , I., Belušic´ , D., 2009. The source of the 2007 Ist meteotsunami (Adriatic Sea). Journal of Geophysical Research 114. doi:10.1029/2008JC005092. Tinti, S., Piatanesi, A., 1996. Numerical simulations of the tsunami induced by the 1627 earthquake affecting Gargano, southern Italy. Journal of Geodynamics 21, 141–160. Tinti, S., Maramai, A., Graziani, L., 2004. The new catalogue of the Italian tsunamis. Natural Hazards 33, 439–465. Vilibic´ , I., 2008. Numerical simulations of the Proudman resonance. Continental Shelf Research 28, 574–581. Vilibic´ , I., Domijan, N., Orlic´ , M., Leder, N., Pasaric´ , M., 2004. Resonant coupling of a traveling air pressure disturbance with the east Adriatic coastal waters. Journal of Geophysical Research 109, C10001. doi:10.1029/2004JC002279. Vilibic´ , I., Šepic´ , J., 2009. Destructive meteotsunamis along the eastern Adriatic coast (overview). Physics and Chemistry of the Earth 34, 904–917. Vucˇetic´ , T., Barcˇot, T., 2008. Records on ‘‘tidal wave” that hit Vela Luka on 21 June 1978. Municipality of Vela Luka and Institute of Oceanography and Fisheries, Vela Luka–Split, 80 pp (in Croatian). Zore-Armanda, M., 1979. Destructive wave in the Adriatic. Rapport et Procèsverbaux des Réunions du Conseil International pour l’Exploration Scientifique de la Mer Méditerranée 25–26, 93–94. T. Vucˇetic´ et al. / Physics and Chemistry of the Earth 34 (2009) 894–903 903en
dc.description.obiettivoSpecifico4.4. Scenari e mitigazione del rischio ambientaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorVucetic, T.en
dc.contributor.authorVilibic, I.en
dc.contributor.authorTinti, S.en
dc.contributor.authorMaramai, A.en
dc.contributor.departmentObala 4, Vela Luka, Croatiaen
dc.contributor.departmentInstitute of Oceanography and Fisheries, Split, Croatiaen
dc.contributor.departmentDip.to di Fisica, Settore Geofisica, University of Bolognaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptObala 4, Vela Luka, Croatia-
crisitem.author.deptInstitute of Oceanography and Fisheries, Split, Croatia-
crisitem.author.deptUniversità di Bologna-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0003-2797-9557-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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