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Reply to "Comment on 'Why Do Modern Probabilistic Seismic-Hazard Analyses Often Lead to Increased Hazard Estimates?' by Julian J. Bommer and Norman A. Abrahamson" by Jens-Uwe KlugelBommer, J. J.; Abrahamson, N. A. · 2007
Why Do Modern Probabilistic Seismic-Hazard Analyses Often Lead to Increased Hazard Estimates?Bommer, J. J.; Abrahamson, N. A. · Bulletin of the Seismological Society of America · 2006
Alternative Approaches to Modeling Epistemic Uncertainty in Ground Motions in Probabilistic Seismic-Hazard AnalysisAtkinson, G. M.; Bommer, J. J.; Abrahamson, N. A. · Seismological Research Letters · 2014
Multiwavelet Seismic-Wave GradiometryPoppeliers, C. · Bulletin of the Seismological Society of America · 2011
Facilitated Estimation of ETASSchoenberg, F. P. · Bulletin of the Seismological Society of America · 2013
Scenario ShakeMaps for Ottawa, CanadaPal, J. D.; Atkinson, G. M. · Bulletin of the Seismological Society of America · 2012
Foreshock Rates from Aftershock AbundanceChristophersen, A.; Smith, E. G. C. · Bulletin of the Seismological Society of America · 2008
Tohoku Earthquake: A Surprise?Kagan, Y. Y.; Jackson, D. D. · Bulletin of the Seismological Society of America · 2013
Frequency Distribution of Felt EarthquakesKato, M. · Bulletin of the Seismological Society of America · 2013
Single-Station SigmaAtkinson, G. M. · Bulletin of the Seismological Society of America · 2006
Wave Gradiometry in Two DimensionsLangston, C. A. · Bulletin of the Seismological Society of America · 2007