2016
DOI: 10.1785/0120150096
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Ground‐Motion Prediction Equations for Region‐Specific Probabilistic Seismic‐Hazard Analysis

Abstract: The goal of this article is to investigate the possibility of reducing the uncertainty of the ground motion predicted for a specific target area (Po Plain and northeastern Italy), by calibrating a set of ad hoc ground-motion prediction equations (GMPEs). The derived GMPEs account for peculiarities that are not generally considered by standard predictive models, such as (1) an attenuation rate dependent on distance ranges and geological domains; (2) enhancement of short-period spectral ordinates, due to the ref… Show more

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Cited by 37 publications
(24 citation statements)
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“…To increase the number of recordings for magnitude between 5 and 6, the calibration data set includes 655 recordings relevant to the 2009 L'Aquila sequence and 233 recordings for the 2012 Emilia sequence (Figures b and c). While we assume that the source scaling in equation is the same for the two sequences (i.e., parameters A and B ), previous studies highlighted peculiarities in the attenuation with distance for the recordings of the Emilia sequence [ Lanzano et al , ]. Therefore, equation is modified by introducing two different sets of attenuation coefficients: CjNI(where NI stands for Northern Italy) and CjCI (where CI stands for Central Italy) for Emilia and L'Aquila recordings, respectively.…”
Section: Iv2 Versus Radiated Energymentioning
confidence: 99%
“…To increase the number of recordings for magnitude between 5 and 6, the calibration data set includes 655 recordings relevant to the 2009 L'Aquila sequence and 233 recordings for the 2012 Emilia sequence (Figures b and c). While we assume that the source scaling in equation is the same for the two sequences (i.e., parameters A and B ), previous studies highlighted peculiarities in the attenuation with distance for the recordings of the Emilia sequence [ Lanzano et al , ]. Therefore, equation is modified by introducing two different sets of attenuation coefficients: CjNI(where NI stands for Northern Italy) and CjCI (where CI stands for Central Italy) for Emilia and L'Aquila recordings, respectively.…”
Section: Iv2 Versus Radiated Energymentioning
confidence: 99%
“…The GMMs discussed above have been applied in several recent PSHA exercises; however, these GMMs have been developed without consideration of the spatial correlation in ground motions, possibly due to the complexity in the estimation process. For instance, Jayaram and Baker developed spatial correlation models for several global earthquakes using the NGA‐West (Next Generation of Ground‐Motion Attenuation Models for the Western US) GMMs (eg, CY08), proposing a predictive model of the effective range parameter trueh˜ (ie, the separation distance between stations at which the spatial correlation is about 0.05) as a function of the structural period T (in seconds).…”
Section: Introduction and Motivationsmentioning
confidence: 99%
“…The between-event standard deviation τ of SI17ref is significantly lower than for ITA10, with a reduction in the range of 40% to 50%. This is expected, as a local dataset is used for the model calibration (see also [64]), and the event metadata in ESM were revised and improved with respect to those used for ITA10. Finally, the within-event variability of SI17ref is larger than for ITA10.…”
Section: Empirical Gmpesmentioning
confidence: 99%