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Taiwan-Specific Model for VS30 Prediction Considering Between-Proxy Correlations

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dc.contributor.authorKwok, On Lei Annie-
dc.contributor.authorStewart, Jonathan P.-
dc.contributor.authorKwak, Dong Youp-
dc.contributor.authorSun, Pang-Li-
dc.date.accessioned2021-06-22T11:22:18Z-
dc.date.available2021-06-22T11:22:18Z-
dc.date.created2021-01-21-
dc.date.issued2018-11-
dc.identifier.issn8755-2930-
dc.identifier.urihttps://scholarworks.bwise.kr/erica/handle/2021.sw.erica/5188-
dc.description.abstractErgodic site response models are generally conditional on the time-averaged shear wave velocity in the upper 30 m (V-S30). Ground motion databases contain many recordings from Taiwan, and because of site characterization efforts, 56% of recording sites have V-S30 derived from measurements. We develop proxy-based V-S30 prediction models, one application of which is for the remaining 44% of Taiwan sites. Our approach, which can be suitable for other regions, differs from previous studies in which proxies are based on detailed geologic categories and possible within-category topographic gradient effects. Instead, we use three broad, age-based geologic categories, and for the youngest category of Holocene and Quaternary undivided sediments, we propose models conditioned on gradient and elevation. We also adapt a geomorphic terrain-based method, thus providing two V-S30-predictionmodels. We describe a model weighting scheme that combines the models in consideration of their relative dispersions and correlation, producing a weighted mean and standard deviation natural-log V-S30. Included as an electronic supplement is a profile database file and a site database with site parameters for Taiwan ground motion stations.-
dc.language영어-
dc.language.isoen-
dc.publisherEarthquake Engineering Research Institute-
dc.titleTaiwan-Specific Model for VS30 Prediction Considering Between-Proxy Correlations-
dc.typeArticle-
dc.contributor.affiliatedAuthorKwak, Dong Youp-
dc.identifier.doi10.1193/061217EQS113M-
dc.identifier.scopusid2-s2.0-85060043256-
dc.identifier.wosid000454334200020-
dc.identifier.bibliographicCitationEarthquake Spectra, v.34, no.4, pp.1973 - 1993-
dc.relation.isPartOfEarthquake Spectra-
dc.citation.titleEarthquake Spectra-
dc.citation.volume34-
dc.citation.number4-
dc.citation.startPage1973-
dc.citation.endPage1993-
dc.type.rimsART-
dc.type.docTypeArticle-
dc.description.journalClass1-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaEngineering-
dc.relation.journalWebOfScienceCategoryEngineering, Civil-
dc.relation.journalWebOfScienceCategoryEngineering, Geological-
dc.subject.keywordPlusWAVE VELOCITY-
dc.subject.keywordPlusSITE CLASSIFICATION-
dc.subject.keywordPlusCALIFORNIA-
dc.subject.keywordPlusMOTION-
dc.subject.keywordPlusV-S30-
dc.subject.keywordPlusPLAIN-
dc.identifier.urlhttps://journals.sagepub.com/doi/10.1193/061217EQS113M-
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ERICA 공학대학 (DEPARTMENT OF CIVIL AND ENVIRONMENTAL ENGINEERING)
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