Abstract

Empirical fragility curves, constructed from databases of thousands of building-damage observations, are commonly used for earthquake risk assessments, particularly in Europe and Japan, where building stocks are often difficult to model analytically (e.g. old masonry structures or timber dwellings). Curves from different studies, however, display considerable differences, which lead to high uncertainty in the assessed seismic risk. One potential reason for this dispersion is the almost universal neglect of the spatial variability in ground motions and the epistemic uncertainty in ground-motion prediction. In this paper, databases of building damage are simulated using ground-motion fields that take account of spatial variability and a known fragility curve. These databases are then inverted, applying a standard approach for the derivation of empirical fragility curves, and the difference with the known curve is studied. A parametric analysis is conducted to investigate the impact of various assumptions on the results. By this approach, it is concluded that ground-motion variability leads to flatter fragility curves and that the epistemic uncertainty in the ground-motion prediction equation used can have a dramatic impact on the derived curves. Without dense ground-motion recording networks in the epicentral area empirical curves will remain highly uncertain. Moreover, the use of aggregated damage observations appears to substantially increase uncertainty in the empirical fragility assessment. In contrast, the use of limited randomly-chosen un-aggregated samples in the affected area can result in good predictions of fragility.

Highlights

  • Fragility curves of buildings exposed to earthquakes express the likelihood of damage to these assets from future seismic events

  • Empirical fragility curves are based on the statistical analysis of post-earthquake observations of the damage sustained by the exposed buildings and the corresponding ground-motion intensity level at the building locations

  • Given the general lack of a dense strong-motion network in the areas of damaging earthquakes, the intensity levels are typically estimated though ground motion prediction equations (GMPEs) or, more recently, ShakeMaps

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Summary

Introduction

Fragility curves of buildings exposed to earthquakes express the likelihood of damage to these assets from future seismic events. Empirical fragility curves are based on the statistical analysis of post-earthquake observations of the damage sustained by the exposed buildings and the corresponding ground-motion intensity level at the building locations. At least 119 empirical fragility curves have been published [1]. These curves have generally been constructed assuming that the measurement error in the intensity-measure levels (IMLs) is negligible. Given the general lack of a dense strong-motion network in the areas of damaging earthquakes, the intensity levels are typically estimated though ground motion prediction equations (GMPEs) or, more recently, ShakeMaps. The impact of this measurement error on empirical fragility curves is not well understood

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