Refinements to the Graves and Pitarka (2010) Broadband Ground-Motion Simulation Method

Abstract

This brief article describes refinements to the Graves and Pitarka (2010) broadband ground‐motion simulation methodology (GP2010 hereafter) that have been implemented in version 14.3 of the Southern California Earthquake Center (SCEC) Broadband Platform (BBP). The updated version of our method on the current SCEC BBP is referred to as GP14.3. Our simulation technique is a hybrid approach that combines low‐ and high‐frequency motions computed with different methods into a single broadband response. The separate low‐ and high‐frequency components have traditionally been called deterministic and stochastic, respectively; however, this nomenclature is an oversimplification. In reality, the low‐frequency approach includes many stochastic elements, and likewise, the high‐frequency approach includes many deterministic elements (e.g., Pulido and Kubo, 2004; Hartzell et al. , 2005; Liu et al. , 2006; Frankel, 2009; Graves and Pitarka, 2010; Mai et al. , 2010). Although the traditional terminology will likely remain in use by the broader modeling community, in this paper we will refer to these using the generic terminology low‐ and high‐frequency approaches. Furthermore, one of the primary goals in refining our methodology is to provide a smoother and more consistent transition between the low‐ and high‐frequency calculations, with the ultimate objective being the development of a single unified modeling approach that can be applied over a broad frequency band. GP2010 was validated by modeling recorded strong motions from four California earthquakes. Although the method performed well overall, several issues were identified including the tendency to overpredict the level of longer period (2–5 s) motions and the effects of rupture directivity. The refinements incorporated in GP14.3 are aimed at addressing these issues with application to the simulation of earthquakes in western United States (WUS). These refinements include the addition of a deep weak zone (details in following section) to the rupture characterization and allowing perturbations in …