Earthquake Early Warning Systems, P. Gasparini et al. editors, Springer, 2007
V. Convertito, R. De Matteis, A. Romeo, A. Zollo and G. Iannaccone
For early-warning applications in particular, the reliability and efficiency of rapid scenario generation strongly depend on the availability of reliable strong ground-motion prediction tools. If shake maps are used to represent patterns of potential damage as a consequence of large earthquakes, attenuation relations are used as tool for predicting peak ground-motion parameters and intensities. One of the limitations in the use of attenuation relations is that these have only rarely been retrieved from data collected in the same tectonic environment in which the prediction have to be performed. As a consequence, strong ground motion can result in underestimations or overestimations with respect to the recorded data. This is true also for the Italian territories, and in
particular for the Southern Apennines, due to limitations in the available databases, both in terms of distances and magnitude. Moreover, for “real-time” early-warning applications, it is important to have attenuation models for which the parameters can be easily upgraded when new data are collected, whether this has to be done during the earthquake rupture occurrence or in the post-event, when the whole strong motion waveforms are available.
In the present study, a strong-motion attenuation relation for early-warning applications in the Campania region (Southern Apennines), Italy, is presented. The model has a classical analytical formulation, and its coefficients were retrieved from a synthetic strong-motion database created by using a stochastic approach. The input parameters for the simulation technique were obtainedthrough the spectral analysis of waveforms of earthquakes recorded by the Istituto Nazionale di Geofisica e Vulacnologia (INGV) network for a magnitude range Md (1.5,5.0) in the last fifteen years, and they have been extrapolated to cover a larger range.
To validate the inferred relation obtained, comparisons with two existing attenuation relations are presented. The results show that the calibration of the attenuation parameters, i.e., geometric spreading, quality factor Q, static stress drop values along with their uncertainties are the main concern.