ABSTRACT
In regions of low-to-moderate seismicity where representative strong motion data is lacking, the modelling of seismic hazard relies on the use of seismological models. This paper presents a set of expressions that can be used as ground motion prediction equations that have been transformed from seismological models which resolve the generation of seismic waves into several components. The feature of this presented set of expressions is that it can be adapted to represent earthquake ground motion behaviour that is defined by a diversity of seismological models. The motivation behind the development of the presented adaptive predictive relationship which is known as the Component Attenuation Model (CAM) was to fast track, and make transparent, the transformation from seismological models to predictions of response spectral values for engineering applications. Thus, CAM can be used to waive away the need of executing any software for undertaking stochastic simulations nor time-history analyses for calculation of the response spectral ordinates. An important and original, the feature of CAM is incorporating the shear wave velocity profile of the bedrock and the associated upper-crustal modification into the model. This article presenting CAM is essentially a contribution to engineering as opposed to seismology. The potential benefits derived from the fast-tracking can be considerable given that the transformation is seldom a one-off process and would need to be repeated for any given targeted area, in view of uncertainties surrounding seismological conditions of the earth crust around the globe.
Acknowledgments
The support of the Commonwealth of Australia through the Cooperative Research Centre program is sincerely acknowledged. The support from the CSC scholarship provided by China Scholarship Council and the Write Up Award provided by The University of Melbourne for the first author is sincerely acknowledged. The guidance of using Swiss earthquake recording data from Earthquake Engineering and Structural Dynamics (EESD) Laboratory in École Polytechnique Fédérale de Lausanne (EPFL) is also sincerely acknowledged. The suggestive comments provided by the two anonymous reviewers are deeply acknowledged as well.
Data And Resources
All the electronic version of the data and MATLAB program scripts can be made available upon requests. The recording data used in this study are obtained from SED (Swiss Seismological Service) Strong Motion Portal (http://strongmotionportal.seismo.ethz.ch/home/, which was last accessed by the authors in January 2019).