Broadband Ground Mo,on Simula,on Plans

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1 Broadband Ground Mo,on Simula,on Plans Paul Somerville URS SCEC Ground Mo5on Simula5on Valida5on Progress Workshop Sept 9, 2012

2 Outline Summary of par5cipa5ng simula5on modules Selec5on of reference velocity and Q models Selec5on of reference source geometry (SRC) Genera5on of mul5ple rupture models (SRF) Running broadband simula5ons Goodness of fit based on best filng rup model Goodness of fit based on average rupture model

3 Par,cipa,ng Simula,on Modules h:p://scec.usc.edu/scecpedia/broadband_pla?orm_mee,ng_- _7_March_2012 GREENS FUNCTION BASED MODELS SDSU Olsen/Mai opera5onal UCSB Archuleta et al opera5onal URS Graves/Pitarka opera5onal Irikura/Miyake asperity source model to be implemented Zeng/Anderson composite source model - to be implemented NON- GREENS FUNCTION BASED MODULES Point source stochas5c model Boore - to be implemented Finite- fault stochas5c model Atkinson - to be implemented GMPE Empirical GMPE with event terms - to be implemented

4 Reference Velocity Models for Green s Func,on Calcula,ons Use regional velocity models for rock site condi5ons e.g. a southern California model e.g. a Japan model Use a standard shallow velocity profile with Vs30 = 863 m/s Data are correc5ons for basin condi5ons using Z1.0 in the C&Y 2008 GMPE

5 Southern California Velocity Models

6 Japan Velocity Models from Koketsu 3D Model of Japan

7 Source Geometry (SRC file) MAGNITUDE = 6.9 FAULT_LENGTH = 40.0 DLEN = xxx FAULT_WIDTH = 17.5 DWID = xxx DEPTH_TO_TOP = 3.85 STRIKE = 128 RAKE = 145 DIP = 70 LAT_TOP_CENTER = LON_TOP_CENTER = HYPO_ALONG_STK = 0.0 HYPO_DOWN_DIP = DT = xxx SEED = xxx CORNER_FREQ = xxx SEISMIC MOMENT = XXX HYPO LAT = xxx HYPO LONG = XXX HYPO DEPTH = XXX

8 Selec,on of Reference SRC Models Review alterna5ve published rupture models (Mai website and newer sources) Retain significant mul5- segment and branching characteris5cs, because one role of the simula5ons it to model these effects because they are hard to represent in GMPE s

9 Earthquake Event List Eq Number YEAR REGION EQ NAME EQID Mul,ple Fault Segments Mar,n Mai Website Author of Reference Model WUS El Mayor Cucapah 280 yes no Wei et al., WUS Northridge 127 no yes Hartzell et al., WUS Hector Mine 158 yes yes Kaverina and Dreger, WUS Landers 125 yes yes Wald & Heaton, WUS WhiLer Narrows 113 no yes Hartzell & Iida, WUS Big Bear 126 no no Jones and Hough, 1995; NGA Event WUS Parkfield 179 no yes Custodio et al., WUS Loma Prieta 118 no yes Wald et al., WUS North Palm Springs 101 no yes Hartzell, WUS Coalinga 76 no no NGA Event WUS San Simeon 177 no no Ji et al., CENA Saguenay CENA- 5 no yes Hartzell et al., CENA Riviere- du- Loup CENA- 32 no no Herrmann CENA Mineral, VA CENA- 88 no no Chapman, JAPAN Tonori 176 no yes Iwata & Sekiguchi, JAPAN Chuetsu- Oki 278 no no Aoi et al., JAPAN Niigata 180 no no Asano & Iwata, JAPAN Iwate 279 no no Yoshida et al., TURKEY Kocaeli 136 yes yes Sekiguchi & Iwata, TAIWAN Chi- Chi 137 yes no Ji et al., ITALY L' Aquila 274 no no Cirella et al., NEW ZEALAND NEW ZEALAND Christchurch 346 yes no Beavan et al., 2012 Darfield 281 yes no Beavan et al, 2012

10 Source Rupture Model (SRF file) Tonori eq: Graves SRF from Iwata and Sekiguchi

11 Approaches to Rupture Modeling Randomly generate 50 SRF s from the SRC Perform simula5ons for each SRF Measure goodness of fit for each SRF PATH 1 Find the best filng SRF Use its goodness of fit to represent modeling uncertainty Include uncertainty in SRF specifica5on when forward modeling future scenarios PATH 2 Use the average goodness of fit of 50 SRF s to represent modeling uncertainty No need to include uncertainty in SRF specifica5on when forward modeling future scenarios

12 Valida,ons: Part A Compare simula5ons to observed ground mo5ons 20 shallow crustal earthquakes (M>6) Set up valida5on exercises for each earthquake Path descrip5on 1- D GF Source descrip5on Simple geometry and mechanism Sets of alterna5ve slip models Site descrip5on Loca5ons Site response factors including non- linear factors Observed ground mo5ons 5% damped response spectral values Arias intensity 5-75% Dura5on Compute bias (mean misfit) and standard devia5on of misfit

13 Valida,ons Part B Compare to empirical GMPEs in range that is well constrained by data M6-7 Distances km Set up valida5on cases M6.0, M6.5, M7.0 R 15, 20, 30, 40, 50 (mul5ple sta5on loca5ons along strike) SS and RV (45 dip) VS30=750 m/s For each case, run forward simula5ons for mul5ple realiza5ons of the source model (e.g ) to give stable es5mates of median and standard devia5on Compute bias (mean misfit) and standard devia5on from simula5ons

14 SCEC Tasks New module development Valida5on Cases Set up the valida5on exercises Part A Part B Conduct valida5on Developers test and revise modules IT support for implementa5on for large suites of forward simula5ons Does not cover costs for person to run simula5ons under QA Review forward simula5on results Workshop with module developers to understand the differences

15 Sponsor Objec,ves Broadband platorm modules Magnitudes: M6 M8 Rupture Distances: 0-15 km Mechanisms: Strike- slip, reverse, normal Frequency Band: 0.1 to 30 Hz (can get by with 5-10 hz if it captures the peak in the accelera5on response spectrum Crustal structure: 1- D Valida5ons (A) test simula5on methods for event- specific source models (op5mized) (B) test method for genera5ng source models for future earthquakes Forward Simula5ons Generate sets of ground mo5ons for large suites of future earthquakes Be able to conduct simula5ons under QA

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