Electronic Supplement to
Ground Motion Modeling of the 1906 San Francisco Earthquake I: Validation Using the 1989 Loma Prieta Earthquake

by Brad T. Aagaard, Thomas M. Brocher, David Dolenc, Douglas Dreger, Robert W. Graves, Stephen Harmsen, Stephen Hartzell, Shawn Larsen, and Mary Lou Zoback

Synthetic versus Long-Period Instrumental Intensities

Duplicates of figures in manuscript comparing synthetic and low-pass filtered instrumental intensities for each of the ground motion modeling groups and the two source models.

Broadband (left) and long-period (right) instrumental ShakeMaps for the 1989 Loma Prieta earthquake. The star identifies the epicenter, the thick black lines delineate the projection of the fault plane in the Wald source model, and the triangles show locations of the stations used in the construction of the ShakeMap.

Broadband Long-Period (T > 1.0 s)
Broadband instrumental ShakeMap Long-period instrumental ShakeMap

Synthetic ShakeMaps for Aagaard's (T > 2.0 s) simulations of the Loma Prieta earthquake with the Beroza and Wald source models. The lower panels show the differences between the synthetic ShakeMaps (top panels) and the long-period (T > 1.0 s) instrumental ShakeMap.

Beroza Source Wald Source
Aagaard, Beroza Source, MMI Aagaard, Wald Source, MMI
Aagaard, Beroza Source, MMI difference Aagaard, Wald Source, MMI difference
Aagaard, Beroza Source, MMI misfit Aagaard, Wald Source, MMI misfit

Synthetic ShakeMaps for Dolenc et al.'s (T > 1.25 s) simulations of the Loma Prieta earthquake with the Beroza and Wald source models. The lower panels show the differences between the synthetic ShakeMaps (top panels) and the long-period (T > 1.0 s) instrumental ShakeMap.

Beroza Source Wald Source
Dolenc, Beroza Source, MMI Dolenc, Wald Source, MMI
Dolenc, Beroza Source, MMI difference Dolenc, Wald Source, MMI difference
Dolenc, Beroza Source, MMI misfit Dolenc, Wald Source, MMI misfit

Synthetic ShakeMaps for Graves's (T > 1.0 s) simulations of the Loma Prieta earthquake with the Beroza and Wald source models. The lower panels show the differences between the synthetic ShakeMaps (top panels) and the long-period (T > 1.0 s) instrumental ShakeMap.

Beroza Source Wald Source
Graves, Beroza Source, MMI Graves, Wald Source, MMI
Graves, Beroza Source, MMI difference Graves, Wald Source, MMI difference
Graves, Beroza Source, MMI misfit Graves, Wald Source, MMI misfit

Synthetic ShakeMaps for Harmsen et al.'s (T > 1.0 s) simulations of the Loma Prieta earthquake with the Beroza and Wald source models. The lower panels show the differences between the synthetic ShakeMaps (top panels) and the long-period (T > 1.0 s) instrumental ShakeMap.

Beroza Source Wald Source
Harmsen, Beroza Source, MMI Harmsen, Wald Source, MMI
Harmsen, Beroza Source, MMI difference Harmsen, Wald Source, MMI difference
Harmsen, Beroza Source, MMI misfit Harmsen, Wald Source, MMI misfit

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