CyberShake Simulations for Path Effects near SONGS · NGA ground motion model for the geometric...
Transcript of CyberShake Simulations for Path Effects near SONGS · NGA ground motion model for the geometric...
Southern California Earthquake Center
CyberShake Simulations for Path Effects near SONGS
Feng Wang, Thomas H. Jordan, Robert Graves, Scott Callaghan, Philip Maechling, and the CME
Collaboration
Southern California Earthquake Center
SCEC’s CyberShake utilizes 3D simulations and finite-fault rupture descriptions to compute deterministic and probabilistic seismic hazard in Southern California. (Graves et al., 2010)
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s758 “San Onofre”
Southern California Earthquake Center
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CyberShake: Simulation-based seismic hazard model
GenSlip v2.1 (Graves and Pitarka, 2007) GenSlip v3.2 (Graves and Pitarka, 2010)
Spatial slip distribution and rupture front
Rise time for slip velocity function
Slip directions (rake distribution)
Rise time
Slip Velocity Function ~7000 fault ruptures (UCERF 2) ~60 realizations per rupture multiple hypocenter locations, and pseudo-dynamic rupture descriptions ~440,000 rupture variations
Southern California Earthquake Center
~7000 fault ruptures (UCERF 2) ~60 realizations per rupture multiple hypocenter locations, and pseudo-dynamic rupture descriptions ~440,000 rupture variations
CyberShake: Simulation-based seismic hazard model
3D velocity structure, e.g. CVM-S4, CVM-Harvard
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Community Velocity Model 4.0, SCEC (CVM-S4)
Southern California Earthquake Center
PGV, PGA, SA Hazard curves and maps
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~108 broadband synthetic seismograms: LF(<0.5 Hz) + HF (up to 10 Hz)
Seismogram synthesis for 235 sites using reciprocity, and stochastic methods (EXSIM)
~7000 fault ruptures (UCERF 2) ~60 realizations per rupture multiple hypocenter locations, and pseudo-dynamic rupture descriptions ~440,000 rupture variations
CyberShake: Simulation-based seismic hazard model
3D velocity structure, e.g. CVM-S4, CVM-Harvard
Southern California Earthquake Center NGA (2008) Attenuation Relations used in National Seismic Hazard Maps
NGA Boore & Atkinson
NGA Chiou & Youngs
NGA Abrahamson & Silva
PoE = 2%/50 yr Source:
http://scec.usc.edu/scecpedia/CyberShake
NGA Campbell & Bozorgnia
CyberShake (2009) Hazard Model
CyberShake shows higher hazard in sedimentary basins relative to NGA GMPEs
Southern California Earthquake Center
Path effects can be explicitly calculated for each CyberShake source
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Southern California Earthquake Center
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Campbell and Bozorgnia
Chiou and Youngs
Abrahamson and Silva
CyberShake
ln (SA) at 3.0 s
Site-specific effects, corrected using Vs30 effects of Boore and Atkinson (2008), are larger in CyberShake model than in other three NGA GMPEs (2008)
Southern California Earthquake Center
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Z2.
5 Z1.
0
Z1.
0
Campbell and Bozorgnia
Chiou and Youngs
Abrahamson and Silva
CyberShake
Not simple function of basin depth
Site-specific effects, corrected using Vs30 effects of Boore and Atkinson (2008), are larger in CyberShake model than in other three NGA GMPEs (2008)
ln (SA) at 3.0 s
Southern California Earthquake Center
Three-dimensional velocity models (CVM-S and CVM-H) have different basin structures around SONGS
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Southern California Earthquake Center
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3s SA
Site s758 San Onofre
PoE: 2% in 50 yr
Annu
al F
requ
ency
of E
xcee
danc
e
by factor of 2
The major source of epistemic uncertainty is the 3D basin structure
Southern California Earthquake Center
CyberShake layered seismic-hazard models
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(Bazzurro and Cornell, 1999)
Southern California Earthquake Center
4 x 10-4 per yr
San Onofre Nuclear Generating Site
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Rose Canyon- Newport-Inglewood
fault Elsinore fault
Disaggregation Diagram
Figure generated using OpenSHA (Field et al. 2003)
Hazard curves
3.0 s SA (g)
s758
Southern California Earthquake Center
4 x 10-5 per year
San Onofre Nuclear Generating Site
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Rose Canyon- Newport-Inglewood
fault Elsinore fault
San Jacinto fault
San Andreas fault
Disaggregation Diagram
Hazard curves
3.0 s SA (g)
s758
Southern California Earthquake Center References
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Abrahamson, N. A. and W. Silva, 2008. Summary of the Abrahamson & Silva NGA Ground-Motion Relations, Earthquake Spectra, 24 (1), 67-97.
Bazzurro, P. and C. A., Cornell, 1999. Disaggregaion of seismic hazard. Bull. Seism. Soc. Am., 89, 2, 501-520. Boore, D. M. and G. M. Atkinson, 2008. Ground-motion prediction equations for the average horizontal component of PGA, PGV,
and 5%-Damped PSA at spectral periods between 0.01s and 10.0s, Earthquake Spectra, 24 (1), 99-138. Campbell, K. W. and Y. Bozorgnia, 2008. NGA ground motion model for the geometric mean horizontal component of PGA, PGV,
PGD and 5% damped linear elastic response spectra for periods ranging from 0.01 to 10s, Earthquake Spectra, 24 (1), 139-171.
Chiou, B. S.-J. and R. R. Youngs, 2008. An NGA model for the average horizontal component of peak ground motion and response spectra, Earthquake Spectra, 24 (1), 173-215.
Field, E. H., T. E. Dawson, K. R. Felzer, A. D. Frankel, V. Gupta, T. H. Jordan, T. Parsons, M. D. Petersen, R. S. Stein, R. J. Weldon II, and C. J. Wills, 2009. Uniform California earthquake rupture forecast, version 2 (UCERF2.0). Bull. Seism. Soc. Am., 99, 2053-2107.
Graves, R., T. H. Jordan, S. Callaghan, E. Deelman, E. H. Field, G. June, C. Kesselman, P. Maechling, G. Mehta, D. Okaya, P. Small, K. Vahi, 2010. CyberShake: A Physics-Based Seismic Hazard Model for Southern California, Pure Appl. Geophys., 168, N 3-4, 367-381.
Graves, R., and A. Pitarka, 2010. Broadband ground-motion simulation using a hybrid approach. Bull. Seism. Soc. Am., 100, 5A, 2095-2013.
Magistrale, H., S. M. Day, R. W. Clayton, and R. W. Graves, 2000. The SCEC Southern California reference three-dimensional seismic velocity model version 2, Bull. Seism. Soc. Am., 90, 6B, S65-S76.
Mai P, Beroza G, 2010. A spatial random field model to characterize complexity in earthquake slip. J. Geophys. Res., 107(B11): doi:10.1029/2001JB000588.
Field, E. H., T. H. Jordan, and C. A. Cornell, 2003. OpenSHA: A developing community-modeling environment for seismic hazard analysis. 74, 4, 406-419.
SCEC wiki: http://scec.usc.edu/scecpedia/CyberShake, last accessed on March 17th, 2013. Suess, M. P., and J. H. Shaw, 2003. P-wave seismic velocity structure derived from sonic logs and industry reflection data in the
Los Angeles basin, California, J. Geoph. Res., 108, B3.