Abstract:Probabilistic seismic hazard analysis (PSHA) is a regularly applied practice that precedes the construction of important engineering structures. The Cornell-McGuire procedure is the most frequently applied method of PSHA. This paper examines the fundamental assumption of the Cornell-McGuire procedure for PSHA, namely, the log-normal distribution of the residuals of the ground motion parameters. Although the assumption of log-normality is standard, it has not been rigorously tested. Moreover, the application of… Show more
“…Although there is no obvious trend, all the estimates of ξ were negative, which confirms the convergence of data to the bounded Weibull extreme value distribution. Similar results were obtained by Huyse et al (2010) and Pavlenko (2015).…”
Section: Resultssupporting
confidence: 89%
“…Huyse et al (2010) applied the peaks over threshold method to analyse both the raw PGA data and the logarithmic residuals of PGA, and concluded that the generalised Pareto distribution (GPD), with the negative shape parameter, provided a model that was more accurate for the tail fractions of both the studied datasets. Similar results were obtained by Pavlenko (2015), who found that the GEVD was a more appropriate model for logarithmic residuals of PGA.…”
The problem considered in this study is that of unrealistic ground motion estimates, which arise in the Cornell-McGuire method when the seismic hazard curve is calculated for extremely low annual probabilities of exceedance. This problem stems from using the normal distribution in the modelling of the variability of the logarithm of ground motion parameters. In this study, the database of the strong-motion seismograph networks of Japan was used to examine the distribution of the logarithm of peak ground acceleration (PGA). The normal distribution and the generalised extreme value distribution (GEVD) models were considered in the analysis, with the preferred model being selected based on statistical criteria. The results of the analysis demonstrated the superiority of the GEVD in the vast majority of considered examples. The estimates of the shape parameter of the GEVD were negative in every considered example, indicating the presence of a finite upper bound of PGA. Therefore, the GEVD provides a model that is more realistic for the scatter of the logarithm of PGA, and the application of this model leads to a bounded seismic hazard curve.
“…Although there is no obvious trend, all the estimates of ξ were negative, which confirms the convergence of data to the bounded Weibull extreme value distribution. Similar results were obtained by Huyse et al (2010) and Pavlenko (2015).…”
Section: Resultssupporting
confidence: 89%
“…Huyse et al (2010) applied the peaks over threshold method to analyse both the raw PGA data and the logarithmic residuals of PGA, and concluded that the generalised Pareto distribution (GPD), with the negative shape parameter, provided a model that was more accurate for the tail fractions of both the studied datasets. Similar results were obtained by Pavlenko (2015), who found that the GEVD was a more appropriate model for logarithmic residuals of PGA.…”
The problem considered in this study is that of unrealistic ground motion estimates, which arise in the Cornell-McGuire method when the seismic hazard curve is calculated for extremely low annual probabilities of exceedance. This problem stems from using the normal distribution in the modelling of the variability of the logarithm of ground motion parameters. In this study, the database of the strong-motion seismograph networks of Japan was used to examine the distribution of the logarithm of peak ground acceleration (PGA). The normal distribution and the generalised extreme value distribution (GEVD) models were considered in the analysis, with the preferred model being selected based on statistical criteria. The results of the analysis demonstrated the superiority of the GEVD in the vast majority of considered examples. The estimates of the shape parameter of the GEVD were negative in every considered example, indicating the presence of a finite upper bound of PGA. Therefore, the GEVD provides a model that is more realistic for the scatter of the logarithm of PGA, and the application of this model leads to a bounded seismic hazard curve.
“…Some tests, such as the LLH test, rely on this assumption. However, the assumption of lognormally distributed residuals has become a de-facto standard and, as a result, usually is not tested routinely for new datasets, but is accepted as a given (Pavlenko, 2015;Raschke, 2013).…”
Section: Advantages and Disadvantages Of The Proposed Metricmentioning
We introduce the cumulative-distribution-based area metric (AM)—also known as stochastic AM—as a scoring metric for earthquake ground-motion models (GMMs). The AM quantitatively informs the user of the degree to which observed or test data fit with a given model, providing a rankable absolute measure of misfit. The AM considers underlying data distributions and model uncertainties without any assumption of form. We apply this metric, along with existing testing methods, to four GMMs in order to test their performance using earthquake ground-motion data from the Preston New Road (United Kingdom) induced seismicity sequences in 2018 and 2019. An advantage of the proposed approach is its applicability to sparse datasets. We, therefore, focus on the ranking of models for discrete ranges of magnitude and distance, some of which have few data points. The variable performance of models in different ranges of the data reveals the importance of considering alternative models. We extend the ranking of GMMs through analysis of intermodel variations of the candidate models over different ranges of magnitude and distance using the AM. We find the intermodel AM can be a useful tool for selection of models for the logic-tree framework in seismic-hazard analysis. Overall, the AM is shown to be efficient and robust in the process of selection and ranking of GMMs for various applications, particularly for sparse and small-sized datasets.
“…The variance of the random component is equal to the residual variance of the regression analysis. However, arguments have been presented against the assumption of the log-normal distribution for the individual random component ε a (Dupuis and Flemming, 2006;Raschke, 2013a;Pavlenko, 2015). Furthermore, the residual variance is not an appropriate estimator for V(ε) because of the principal of area equivalence, as was revealed by Raschke (2013a).…”
In this paper, I introduce a novel approach to modelling the individual random component (also called the intraevent uncertainty) of a ground-motion relation (GMR), as well as a novel approach to estimating the corresponding parameters. In essence, I contend that the individual random component is reproduced adequately by a simple stochastic mechanism of random impulses acting in the horizontal plane, with random directions.
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