2017
DOI: 10.1193/081716eqs135m
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Non-Ergodic Site Response in Seismic Hazard Analysis

Abstract: Probabilistic seismic hazard analyses are usually performed with semi-empirical ground motion models (GMMs) following the ergodic assumption whereby average source, path, and site effects from global databases apply for a specific site of interest. Site-specific site response is likely to differ from the global average conditional on site parameters used in GMMs (typically V S30 and basin depth). Non-ergodic site response can be evaluated using on-site ground motion recordings and/or one-dimensional wave propa… Show more

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Cited by 90 publications
(55 citation statements)
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“…We prefer the use of empirical model trends to guide our extrapolation here rather than simulation results due to difficulties in modeling site response with 1D GRA at long periods (e.g. Stewart et al, 2017a). For V 1 , we maintain the value at 5.0 s for longer periods.…”
Section: Fv Model Developmentmentioning
confidence: 99%
“…We prefer the use of empirical model trends to guide our extrapolation here rather than simulation results due to difficulties in modeling site response with 1D GRA at long periods (e.g. Stewart et al, 2017a). For V 1 , we maintain the value at 5.0 s for longer periods.…”
Section: Fv Model Developmentmentioning
confidence: 99%
“…Let us assume that the uncertainty in the ground motion representation, manifesting itself as the record‐to‐record variability in structural response given the seismic intensity level, is the only source of uncertainty (neglecting modelling uncertainties). Then, neglecting the non ergodicity in seismic hazard assessment, deterioration in structural properties due to aging, and assuming that the damaged structure is always restored to the same intact structure, the LS excursion can be described by a homogenous Poisson distribution. Therefore, Equations and can be used to calculate the structural reliability.…”
Section: Reliability Assessmentmentioning
confidence: 99%
“…This assumption overlooks the site-specific geologies that can influence earthquake ground motion characteristics. While efforts are underway [5][6][7] to develop nonergodic GMMs to better capture local geologic features, their development is limited by the scarcity of strong ground motion records.…”
mentioning
confidence: 99%