- journal_title：Bulletin of the Seismological Society of America
- Contributor：C. B. Worden ; D. J. Wald ; T. I. Allen ; K. Lin ; D. Garcia ; G. Cua
- Publisher：Seismological Society of America
- Date：2010-
- Format：text/html
- Language：en
- Identifier：10.1785/0120100101
- journal_abbrev：Bulletin of the Seismological Society of America
- issn：0037-1106
- volume：100
- issue：6
- firstpage：3083
- section：Articles
We describe a weighted-average approach for incorporating various types of data (observed peak ground motions and intensities and estimates from ground-motion prediction equations) into the ShakeMap ground motion and intensity mapping framework. This approach represents a fundamental revision of our existing ShakeMap methodology. In addition, the increased availability of near-real-time macroseismic intensity data, the development of new relationships between intensity and peak ground motions, and new relationships to directly predict intensity from earthquake source information have facilitated the inclusion of intensity measurements directly into ShakeMap computations. Our approach allows for the combination of (1) direct observations (ground-motion measurements or reported intensities), (2) observations converted from intensity to ground motion (or vice versa), and (3) estimated ground motions and intensities from prediction equations or numerical models. Critically, each of the aforementioned data types must include an estimate of its uncertainties, including those caused by scaling the influence of observations to surrounding grid points and those associated with estimates given an unknown fault geometry. The ShakeMap ground-motion and intensity estimates are an uncertainty-weighted combination of these various data and estimates. A natural by-product of this interpolation process is an estimate of total uncertainty at each point on the map, which can be vital for comprehensive inventory loss calculations. We perform a number of tests to validate this new methodology and find that it produces a substantial improvement in the accuracy of ground-motion predictions over empirical prediction equations alone.