Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7218
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dc.contributor.authorallSandri, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallJolly, G.; GNS Science, Wairakei Research Centre, Taupo, New Zealanden
dc.contributor.authorallLindsay, J.; Institute of Earth Science and Engineering, The University of Auckland, Auckland, New Zealand; School of Environment, The University of Auckland, Auckland, New Zealanden
dc.contributor.authorallHowe, T.; Institute of Earth Science and Engineering, The University of Auckland, Auckland, New Zealanden
dc.contributor.authorallMarzocchi, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2011-12-01T07:52:10Zen
dc.date.available2011-12-01T07:52:10Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/7218en
dc.description.abstractBy using BET_VH, we propose a quantitative probabilistic hazard assessment for base surge impact in Auckland, New Zealand. Base surges resulting from phreatomagmatic eruptions are among the most dangerous phenomena likely to be associated with the initial phase of a future eruption in the Auckland Volcanic Field. The assessment is done both in the long-term and in a specific short-term case study, i.e. the simulated pre-eruptive unrest episode during Exercise Ruaumoko, a national civil defence exercise. The most important factors to account for are the uncertainties in the vent location (expected for a volcanic field) and in the run-out distance of base surges. Here, we propose a statistical model of base surge run-out distance based on deposits from past eruptions in Auckland and in analogous volcanoes. We then combine our hazard assessment with an analysis of the costs and benefits of evacuating people (on a 1km x 1km cell grid). In addition to stressing the practical importance of a cost-benefit analysis in creating a bridge between volcanologists and decision makers, our study highlights some important points. First, in the Exercise Ruaumoko application, the evacuation call seems to be required as soon as the unrest phase is clear; additionally, the evacuation area is much larger than what is recommended in the current Contingency Plan. Secondly, the evacuation area changes in size with time, due to a reduction in the uncertainty in the vent location and increase in the probability of eruption. It is the tradeoff between these two factors that dictates which cells must be evacuated, and when, thus determining the ultimate size and shape of the area to be evacuated.en
dc.language.isoEnglishen
dc.publisher.nameSpringer Berlin Heidelbergen
dc.relation.ispartofBulletin of volcanologyen
dc.relation.ispartofseries/74(2012)en
dc.subjectAuckland Volcanic Fielden
dc.subjectBase surgeen
dc.subjectBayesian event treeen
dc.subjectVolcanic hazarden
dc.subjectCost benefit analysisen
dc.titleCombining long- and short-term probabilistic volcanic hazard assessment with cost-benefit analysis to support decision making in a volcanic crisis from the Auckland Volcanic Field, New Zealanden
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber705-723en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.identifier.doi10.1007/s00445-011-0556-yen
dc.description.obiettivoSpecifico4.3. TTC - Scenari di pericolosità vulcanicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.relation.issn0258-8900en
dc.relation.eissn1432-0819en
dc.contributor.authorSandri, L.en
dc.contributor.authorJolly, G.en
dc.contributor.authorLindsay, J.en
dc.contributor.authorHowe, T.en
dc.contributor.authorMarzocchi, W.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentGNS Science, Wairakei Research Centre, Taupo, New Zealanden
dc.contributor.departmentInstitute of Earth Science and Engineering, The University of Auckland, Auckland, New Zealand; School of Environment, The University of Auckland, Auckland, New Zealanden
dc.contributor.departmentInstitute of Earth Science and Engineering, The University of Auckland, Auckland, New Zealanden
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, 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.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptGNS Science, Wairakei Research Centre, Taupo, New Zealand-
crisitem.author.deptUniversity of Auckland Auckland, NEW ZEALAND-
crisitem.author.deptInstitute of Earth Science and Engineering, The University of Auckland, Auckland, New Zealand-
crisitem.author.orcid0000-0002-3254-2336-
crisitem.author.orcid0000-0003-1413-2541-
crisitem.author.orcid0000-0002-9114-1516-
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-
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