Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6773
AuthorsHainzl, S.* 
Enescu, B.* 
Cocco, M.* 
Woessner, J.* 
Catalli, F.* 
Wang, R.* 
Roth, F.* 
TitleAftershock modeling based on uncertain stress calculations
Issue Date2009
Series/Report no./114 (2009)
DOI10.1029/2008JB006011
URIhttp://hdl.handle.net/2122/6773
Keywordsrate dependent and state dependent frictional model
seismicity
earthquake forecasting
Coulomb stress change
Subject Classification04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution 
04. Solid Earth::04.06. Seismology::04.06.02. Earthquake interactions and probability 
AbstractWe discuss the impact of uncertainties in computed coseismic stress perturbations on the seismicity rate changes forecasted through a rate- and state-dependent frictional model. We aim to understand how the variability of Coulomb stress changes affects the correlation between predicted and observed changes in the rate of earthquake production. We use the aftershock activity following the 1992 M7.3 Landers (California) earthquake as a case study. To accomplish these tasks, we first analyze the variability of stress changes resulting from the use of different published slip distributions. We find that the standard deviation of the uncertainty is of the same size as the absolute stress change and that their ratio, the coefficient of variation (CV), is approximately constant in space. This uncertainty has a strong impact on the forecasted aftershock activity if a rate-and-state frictional model is considered. We use the early aftershocks to invert for friction parameters and the coefficient of variation by means of the maximum likelihood method. We show that, when the uncertainties are properly taken into account, the inversion yields stable results, which fit the spatiotemporal aftershock sequence. The analysis of the 1992 Landers sequence demonstrates that accounting for realistic uncertainties in stress changes strongly improves the correlation between modeled and observed seismicity rate changes. For this sequence, we measure a friction parameter Aσn ≈ 0.017 MPa and a coefficient of stress variation CV = 0.95.
DescriptionAn edited version of this paper was published by AGU. Copyright (2009) American Geophysical Union.
Appears in Collections:Papers Published / Papers in press

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