Electronic Supplement to
Ground
Motion Modeling of the 1906 San Francisco Earthquake I:
Validation Using the 1989 Loma Prieta Earthquake
Comparison of synthetic intensities among the four ground motion modeling groups (Aagaard, Dolenc et al., Graves, and Harmsen et al.) for the Wald and Beroza source models.
Difference in MMI between Aagaard's (T > 2.0 s) simulations and Dolenc at al.'s (T > 1.25 s) simulations of the Loma Prieta earthquake for the Beroza and Wald source models.
Beroza Source | Wald Source |
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Difference in MMI between Harmsen et al.'s (T > 1.0 s) simulations and Dolenc at al.'s (T > 1.25 s) simulations of the Loma Prieta earthquake for the Beroza and Wald source models.
Beroza Source | Wald Source |
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Difference in MMI between Aagaard's (T > 2.0 s) simulations and Graves's (T > 1.0 s) simulations of the Loma Prieta earthquake for the Beroza and Wald source models.
Beroza Source | Wald Source |
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Difference in MMI between Dolenc et al.'s (T > 1.25 s) simulations and Graves's (T > 1.0 s) simulations of the Loma Prieta earthquake for the Beroza and Wald source models.
Beroza Source | Wald Source |
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Difference in MMI between Harmsen et al.'s (T > 1.0 s) simulations and Graves's (T > 1.0 s) simulations of the Loma Prieta earthquake for the Beroza and Wald source models.
Beroza Source | Wald Source |
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Difference in MMI between Graves long-period (T > 1.0 s) and broadband (T > 0.1 s) simulations of the Loma Prieta earthquake for the Beroza and Wald source models.
Beroza Source | Wald Source |
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