Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6515
DC FieldValueLanguage
dc.contributor.authorallBindi, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Milano-Pavia, Milano, Italiaen
dc.contributor.authorallMayfield, M.; GFZ-Potsdamen
dc.contributor.authorallParolai, S.; GFZ-Potsdamen
dc.contributor.authorallTyagunov, S.; KIT-Karlsruheen
dc.contributor.authorallBegaliev, U. T.; INTUIT-Bishkeken
dc.contributor.authorallAbdrakhmatov, K.; KIS-Bishekeken
dc.contributor.authorallMoldobekov, B.; CAIAG-Bishkeken
dc.contributor.authorallZschau, J.; GFZ-Potsdamen
dc.date.accessioned2011-01-11T08:40:31Zen
dc.date.available2011-01-11T08:40:31Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/6515en
dc.description.abstractA risk scenario for Bishkek, capital of the Kyrgyz Republic, is evaluated by considering a magnitude 7.5 earthquake occurring over the Issyk-Ata fault.The intensity values predicted through the application of an attenuation relationship and a recently compiled vulnerability composition model are used as inputs for seismic risk assessment, carried out using the CREST (Cedim Risk Estimation Tool) code. Although the results of this study show a reduction by as much as a factor of two with respect to the results of earlier studies, the risk scenario evaluated in this paper confirms the large number of expected injuries and fatalities in Bishkek, as well as the severe level of building damage. Furthermore, the intensity map has also been evaluated by performing stochastic simulations. The spectral levels of the ground shaking are converted into intensity values by applying a previously derived conversion technique. The local site effects are empirically estimated considering the spectral ratios between the earthquakes recorded by a temporary network deployed in Bishkek and the recordings at two reference sites. Although the intensities computed via stochastic simulations are lower than those estimated with the attenuation relationship, the simulations showed that site effects, which can contribute to intensity increments as large as 2 units in the north part of the town, are playing an important role in altering the risk estimates for different parts of the town.en
dc.language.isoEnglishen
dc.relation.ispartofSoil dynamics and earthquake engineeringen
dc.relation.ispartofseries3/31 (2011)en
dc.subjectseismic risken
dc.titleTowards an improved seismic risk scenario for Bishkek, Kyrgyz Republicen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber521-525en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.identifier.doi10.1016/j.soildyn.2010.08.009en
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorBindi, D.en
dc.contributor.authorMayfield, M.en
dc.contributor.authorParolai, S.en
dc.contributor.authorTyagunov, S.en
dc.contributor.authorBegaliev, U. T.en
dc.contributor.authorAbdrakhmatov, K.en
dc.contributor.authorMoldobekov, B.en
dc.contributor.authorZschau, J.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italiaen
dc.contributor.departmentGFZ-Potsdamen
dc.contributor.departmentGFZ-Potsdamen
dc.contributor.departmentKIT-Karlsruheen
dc.contributor.departmentINTUIT-Bishkeken
dc.contributor.departmentCAIAG-Bishkeken
dc.contributor.departmentGFZ-Potsdamen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptGFZ-Potsdam-
crisitem.author.deptOGS - Istituto Nazionale di Oceanografia e di Geofisica Sperimentale-
crisitem.author.deptKIT-Karlsruhe-
crisitem.author.deptINTUIT-Bishkek-
crisitem.author.deptCAIAG-Bishkek-
crisitem.author.deptDepartment 2: Physics of the Earth, Helmholtz Centre Potsdam, GFZ German Research Centre for Geoscience, Telegrafenberg, 14473 Potsdam, Germany-
crisitem.author.orcid0000-0002-8619-2220-
crisitem.author.orcid0000-0002-9084-7488-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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