Seismic wave amplification by topographic features: A parametric study: Fid-Bau Portal

Seismic wave amplification by topographic features: A parametric study

Poursartip, Babak / Fathi, Arash / Kallivokas, Loukas F.

AbstractDespite the ever increasing adoption of wave motion simulations for assessing seismic hazard, most assessment/simulations are still based on a flat surface earth model. The purpose of this paper is to quantify the effect of topographic irregularities on the ground motion and local site response by means of parametric investigations in the frequency-domain of typical two-dimensional features.To this end, we deploy best-practice tools for simulating seismic events in arbitrarily heterogeneous formations; these include: a forward wave simulator based on a hybrid formulation encompassing perfectly-matched-layers (PMLs); unstructured spectral elements for spatial discretization; and the Domain-Reduction-Method that permits placement of the seismic source within the computational domain, thus allowing consideration of realistic seismic scenarios.Of particular interest to this development is the study of the effects that various idealized topographic features have on the surface motion when compared against the response that is based on a flat-surface assumption. We report the results of parametric studies for various parameters, which show motion amplification that depends, as expected, on the relation between the topographic feature's characteristics and the dominant wavelength. More interestingly, we also report motion de-amplification patterns.

Highlights•Motion amplification is stronger at wavelengths comparable to the feature's size.•Motion amplification is weaker for terrain depressions than for protruding features.•Small variations in geometry modeling may lead to major differences in amplification.•De-amplification is possible to occur within or away from the topographic feature.•Motion amplification tends to be stronger in steeper than in flatter hills.