2010
DOI: 10.3319/tao.2010.05.03.01(t)
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Uncertainty and Spatial Correlation of Earthquake Ground Motion in Taiwan

Abstract: In this work we analyzed characteristics of aleatory variability with regard to intra-event and inter-event components in the prediction of peak ground acceleration in Taiwan and the spatial (site-to-site) correlation of ground motion residuals. The characteristics are very important for an assessment of seismic hazard and loss for regionally located building assets (portfolio) and spatially distributed systems (lifelines) and ShakeMap generation. The strong-motion database collected by the TSMIP network in Ta… Show more

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Cited by 63 publications
(51 citation statements)
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“…Boore et al 2003; Wang and Takada 2005;Sokolov et al 2010), and that the distances over which the correlations may be significant are generally greater for the long period characteristics of the ground motion (Jayaram and Baker 2009). In recent years these observations have proceeded to form the basis for the development of models of spatial cross-correlation to describe the correlation between different ground motion IMs across sites separated over a distance (e.g.…”
Section: Introductionmentioning
confidence: 94%
“…Boore et al 2003; Wang and Takada 2005;Sokolov et al 2010), and that the distances over which the correlations may be significant are generally greater for the long period characteristics of the ground motion (Jayaram and Baker 2009). In recent years these observations have proceeded to form the basis for the development of models of spatial cross-correlation to describe the correlation between different ground motion IMs across sites separated over a distance (e.g.…”
Section: Introductionmentioning
confidence: 94%
“…Europe, such as Northridge (1994) or Chi-Chi (1999). A few works have, instead, combined data from multiple events to obtain a unique estimate of correlation (e.g., 2008a, Goda andAtkinson, 2009;Goda and Atkinson, 2010;Sokolov et al, 2010). Different authors, for a given IM, provide different distance limits for correlation to disappear (i.e., distance beyond which IMs may be considered uncorrelated), and this is supposed to depend on the dataset considered, the GMPE chosen to compute residuals, and the working assumptions of the estimation.…”
Section: Introductionmentioning
confidence: 98%
“…For example, Goda and Atkinson (2009) investigated the effects of earthquake types (i.e., shallow and deep events) on correlation using datasets from K-NET and KiK-net Japanese strong-motion networks without finding any significant dependency. On the other hand, Sokolov et al (2010), starting from the strong-motion database of Taiwan Strong Motion Instrumentation Program (TSMIP) network, estimated correlation for various areas, site classes, and geological structures, asserting that a single generalized spatial model may not be adequate for all of Taiwan territory.…”
Section: Introductionmentioning
confidence: 99%
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“…The integration of seismicity from different earthquake sources that is expressed in the form of conventional seismic hazard maps, is not applicable for the case of the post-earthquake traffic distribution, as the latter depends on the individual probability of operation of each network key component, which is in turn dependent on the specific seismic scenario examined and the corresponding spatial distribution of the Intensity Measures (IM) of interest [12], [13]. For this reason, hazard is herein assessed independently for each one of the m seismic sources potentially affecting the network and for a set of n different return periods.…”
Section: Seismic Hazard Analysismentioning
confidence: 99%