GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 2.1 GNGTS 2024 Figure 3: Distribution of a) between events residuals for Bommer, et al., (2009) model, b) site-to-site residuals for Bommer, et al., (2009) model, c) event-and-site residuals for Bommer, et al., (2009) model, d) between events residuals for Afshari & Stewart, (2016) model, e) site-to-site residuals for Afshari & Stewart, (2016) model, f) event-and site residuals for Afshari & Stewart, (2016) model, g) between events residuals for Tafreshi and Bora (2023) model, h) site-to-site residuals for Tafreshi and Bora (2023) model, i) event-and-site residuals for Tafreshi and Bora (2023) model. References Afshari K., and Stewart J. P.; (2016): Physically Parameterized Prediction Equations for Significant Duration in Active Crustal Regions. Earthquake Spectra, 29. Al Atik L., Abragamson N., Bommer JJ., Scherbaum F., Cotton F., Kuehn N., The variability of ground-motion prediction models and its components. Seismol Res Lett. 2010;81(5):794-801. Ancheta T. D., Darragh R. B., Stewart J. P., Seyhan E., Silva W. J., Chiou B. S.-J., Wooddell K. E., et al.; (2014): NGA-West2 Database. Earthquake Spectra, 30, 989–1005. Bommer J. J., Stafford P. J., and Alarcón, J. E.; (2009): Empirical Equations for the Prediction of the Significant, Bracketed, and Uniform Duration of Earthquake Ground Motion. Bulletin of the Seismological Society of America, 99(6), 3233.