A regional ground motion excitation/attenuation model for the San Francisco region
By using small-to-moderate-sized earthquakes located within ~200 km of San Francisco, we characterize the scaling of the ground motions for frequencies ranging between 0.25 and 20 Hz, obtaining results for geometric spreading, Q(f), and site parameters using the methods of Mayeda et al. (2005) and M...
Published in: | Bulletin of the Seismological Society of America |
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Online Access: | http://hdl.handle.net/2122/2913 http://hdl.handle.net/2122/2306 https://doi.org/10.1785/0120060101 |
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ftingv:oai:www.earth-prints.org:2122/2913 2023-05-15T16:02:09+02:00 A regional ground motion excitation/attenuation model for the San Francisco region Malagnini, L. Mayeda, K. Uhrhammer, R. Akinci, A. Herrmann, R. B. Malagnini, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia Mayeda, K.; Weston Geophysical Corporation Uhrhammer, R.; University of California Berkeley Akinci, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia Herrmann, R. B.; Saint Louis University Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia Weston Geophysical Corporation University of California Berkeley #PLACEHOLDER_PARENT_METADATA_VALUE# 2007-06 http://hdl.handle.net/2122/2913 http://hdl.handle.net/2122/2306 https://doi.org/10.1785/0120060101 en eng Seismological Society of America Bulletin of the Seismological Society of America 3 / 97 (2007) http://hdl.handle.net/2122/2913 http://hdl.handle.net/2122/2306 doi:10.1785/0120060101 open ground motion San Francisco site effects 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion article 2007 ftingv https://doi.org/10.1785/0120060101 2022-07-29T06:04:36Z By using small-to-moderate-sized earthquakes located within ~200 km of San Francisco, we characterize the scaling of the ground motions for frequencies ranging between 0.25 and 20 Hz, obtaining results for geometric spreading, Q(f), and site parameters using the methods of Mayeda et al. (2005) and Malagnini et al. (2004). The results of the analysis show that, throughout the Bay Area, the average regional attenuation of the ground motion can be modeled with a bilinear geometric spreading function with a 30 km crossover distance, coupled to an anelastic function exp(-pi*f*r/V*Q(f)) , where: Q(f)=180f^0.42. A body-wave geometric spreading, g(r)= r^-1.0, is used at short hypocentral distances (r < 30 km), whereas g(r)= r^-0.6 fits the attenuation of the spectral amplitudes at hypocentral distances beyond the crossover. The frequency-dependent site effects at 12 of the Berkeley Digital Seismic Network (BDSN) stations were evaluated in an absolute sense using coda-derived source spectra. Our results show: i) the absolute site response for frequencies ranging between 0.3 Hz and 2.0 Hz correlate with independent estimates of the local magnitude residuals (dML) for each of the stations; ii) moment-magnitudes (MW) derived from our path and site-corrected spectra are in excellent agreement with those independently derived using full-waveform modeling as well as coda-derived source spectra; iii) we use our weak-motion-based relationships to predict motions region wide for the Loma Prieta earthquake, well above the maximum magnitude spanned by our data set, on a completely different set of stations. Results compare well with measurements taken at specific NEHRP site classes; iv) an empirical, magnitude-dependent scaling was necessary for the Brune stress parameter in order to match the large magnitude spectral accelerations and peak ground velocities with our weak-motion-based model. Published 843-862 4.1. Metodologie sismologiche per l'ingegneria sismica JCR Journal partially_open Article in Journal/Newspaper DML Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Brune ENVELOPE(6.723,6.723,62.526,62.526) Loma ENVELOPE(-58.983,-58.983,-62.267,-62.267) Bulletin of the Seismological Society of America 97 3 843 862 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
ground motion San Francisco site effects 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion |
spellingShingle |
ground motion San Francisco site effects 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion Malagnini, L. Mayeda, K. Uhrhammer, R. Akinci, A. Herrmann, R. B. A regional ground motion excitation/attenuation model for the San Francisco region |
topic_facet |
ground motion San Francisco site effects 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion |
description |
By using small-to-moderate-sized earthquakes located within ~200 km of San Francisco, we characterize the scaling of the ground motions for frequencies ranging between 0.25 and 20 Hz, obtaining results for geometric spreading, Q(f), and site parameters using the methods of Mayeda et al. (2005) and Malagnini et al. (2004). The results of the analysis show that, throughout the Bay Area, the average regional attenuation of the ground motion can be modeled with a bilinear geometric spreading function with a 30 km crossover distance, coupled to an anelastic function exp(-pi*f*r/V*Q(f)) , where: Q(f)=180f^0.42. A body-wave geometric spreading, g(r)= r^-1.0, is used at short hypocentral distances (r < 30 km), whereas g(r)= r^-0.6 fits the attenuation of the spectral amplitudes at hypocentral distances beyond the crossover. The frequency-dependent site effects at 12 of the Berkeley Digital Seismic Network (BDSN) stations were evaluated in an absolute sense using coda-derived source spectra. Our results show: i) the absolute site response for frequencies ranging between 0.3 Hz and 2.0 Hz correlate with independent estimates of the local magnitude residuals (dML) for each of the stations; ii) moment-magnitudes (MW) derived from our path and site-corrected spectra are in excellent agreement with those independently derived using full-waveform modeling as well as coda-derived source spectra; iii) we use our weak-motion-based relationships to predict motions region wide for the Loma Prieta earthquake, well above the maximum magnitude spanned by our data set, on a completely different set of stations. Results compare well with measurements taken at specific NEHRP site classes; iv) an empirical, magnitude-dependent scaling was necessary for the Brune stress parameter in order to match the large magnitude spectral accelerations and peak ground velocities with our weak-motion-based model. Published 843-862 4.1. Metodologie sismologiche per l'ingegneria sismica JCR Journal partially_open |
author2 |
Malagnini, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia Mayeda, K.; Weston Geophysical Corporation Uhrhammer, R.; University of California Berkeley Akinci, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia Herrmann, R. B.; Saint Louis University Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia Weston Geophysical Corporation University of California Berkeley #PLACEHOLDER_PARENT_METADATA_VALUE# |
format |
Article in Journal/Newspaper |
author |
Malagnini, L. Mayeda, K. Uhrhammer, R. Akinci, A. Herrmann, R. B. |
author_facet |
Malagnini, L. Mayeda, K. Uhrhammer, R. Akinci, A. Herrmann, R. B. |
author_sort |
Malagnini, L. |
title |
A regional ground motion excitation/attenuation model for the San Francisco region |
title_short |
A regional ground motion excitation/attenuation model for the San Francisco region |
title_full |
A regional ground motion excitation/attenuation model for the San Francisco region |
title_fullStr |
A regional ground motion excitation/attenuation model for the San Francisco region |
title_full_unstemmed |
A regional ground motion excitation/attenuation model for the San Francisco region |
title_sort |
regional ground motion excitation/attenuation model for the san francisco region |
publisher |
Seismological Society of America |
publishDate |
2007 |
url |
http://hdl.handle.net/2122/2913 http://hdl.handle.net/2122/2306 https://doi.org/10.1785/0120060101 |
long_lat |
ENVELOPE(6.723,6.723,62.526,62.526) ENVELOPE(-58.983,-58.983,-62.267,-62.267) |
geographic |
Brune Loma |
geographic_facet |
Brune Loma |
genre |
DML |
genre_facet |
DML |
op_relation |
Bulletin of the Seismological Society of America 3 / 97 (2007) http://hdl.handle.net/2122/2913 http://hdl.handle.net/2122/2306 doi:10.1785/0120060101 |
op_rights |
open |
op_doi |
https://doi.org/10.1785/0120060101 |
container_title |
Bulletin of the Seismological Society of America |
container_volume |
97 |
container_issue |
3 |
container_start_page |
843 |
op_container_end_page |
862 |
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1766397747036946432 |