Linda Al A)k Sigma WG. Jack Baker, Ken Campbell, Brian Chiou, Ellen Rathje, Adrian Rodriguez- Marek, Melanie Walling. Outline
|
|
- Emery Roberts
- 6 years ago
- Views:
Transcription
1 /5/4 SSHAC Level 3 NGA- East Project WS- 2C/3A, October 29-3, 24 Berkeley, CA Preliminary Tau,, and Models for CENA Linda Al A)k Sigma WG Jack Baker, Ken Campbell, Brian Chiou, Ellen Rathje, Adrian Rodriguez- Marek, Melanie Walling Outline General TI Team approach for sigma logic tree Background; ObjecIves; General Approach Preliminary results for CENA data analysis Data distribuion, GMPE funcional form, and residual plots Analysis results for Tau,, and and comparisons Candidate sigma models New preliminary CENA models for Tau,, and ExisIng models 2
2 /5/4 ObjecIves for NGA- East Develop standard deviaion models for ground moion (PSA) applicable for CENA for: Between- event standard deviaion, Tau Ergodic within- event standard deviaion, Single- staion within- event standard deviaion, Models applicable for M 4. to 8.2; distance up to, km; hardrock sites; PGA, PGV and T. to sec 3 General Approach Analysis of residuals of CENA data with respect to developed GMPE to evaluate trends:, distance, V S3 dependence, closeness index Compare CENA,, and Tau to exising models at common magnitudes (<5.8) to inform CENA models at larger M ExisIng models: NGA- West2 models, European models, other Develop new models and evaluate exising models 4 2
3 /5/4 Residual Components δ = δb + δw δ es e es B e : Between- event (inter- event) residual for earthquake e δ W : Within- event (intra- event) es residual at staion s for earthquake e Ala)k et al. (2) 2 2 σ = τ + φ τ : Between- event standard deviaion φ : Within- event standard deviaion 5 Overview of Single- StaIon Given muliple recordings of GM at an individual site, S, allows esimaing the systemaic site effects, δ S2S S, and removing them from the GM variability: Single- Sta-on δ S2S S represents the systemaic deviaion of the observed amplificaion at this site from the median amplificaion predicted by the model δs2s s = Nbofeqks s Nbofeqk s e= δw es Nbofsta s= φ S2S = ( δ S2S ) 2 s Nbofeqk s Nbofsta Nbofeqk s ( δws ) 2 es s= e= φ SS Nbofsta = Nbofeqks s= φ = φ + φ 2 2 SS S 2S 6 3
4 /5/4 Summary of Terminology Residual Between- event residual, δ B e Within- event residual, δ W es Standard Devia)on Between- event standard deviaion, τ=sd(δ B e ) Within- event standard deviaion, φ=sd(δ W es ) Site- to- site residual (site term), δs2 S s Site- to- site variability, φ S2S =SD(δS2 S s ) Single- staion within- event residual, δw S es Single- staion within- event standard deviaion, φ ss =SD(δW S es ) Total (ergodic) standard deviafon: σ= φ 2 + τ 2 Single- stafon standard deviafon (parfally non- ergodic): σ SS = φ ss 2 + τ 2 Al AIk et al. (2) 7 PRELIMINARY RESULTS FOR CENA DATA ANALYSIS: - Data distribu-on, GMPE func-onal form, and residual plots - Analysis results for Tau,, and and comparisons 8 4
5 /5/4 CENA Data DistribuIon at T.sec (Min of 5 recs/eqk) Total: 3,933 recs 65 eqks 746 staions PIE:,849 recs eqks 424 staions 9 CENA Data DistribuIon at T.sec (cont d) 27 staions with < 3 recs 5
6 /5/4 CENA Data DistribuIon (cont d) 2: Paths contained within CUS, Canada (3,44 recs) 3: Paths contained within Appalachian (7 recs) 4: Paths contained within AtlanIc Coast (9 recs) 5: Paths crossing 2, 3, 4 (69 recs) Preliminary CENA Model (PSA) R rup < 5km R rup 5km ln ( ) Y c c M c M 2 = ( rup + ) + rup + + ln ( S ) c ln R c c R c c V ( ) a ( ) ln Y = c c ln 5 + c + c M + c M ( c + c ) ln ( R + c ) + c R + c + c ln ( V ) 4 4a rup 6 7 rup 6 8 S 3 Regression done for distances up to, km. Does not include Gulf region. 2 6
7 /5/4 Between- Event Residual Plots 3 Between- Event Residual Plots (cont d) 4 7
8 /5/4 Within- Event Residual Plots vs. Distance T. sec T. sec 5 Within- Event Residual Plots vs. V S3 T. sec T. sec 6 8
9 /5/4 Within- Event Residual Plots by Region 2: Paths contained within CUS, Canada 3: Paths contained within Appalachian 4: Paths contained within AtlanIc Coast 5: Paths crossing 2, 3, 4 7 PRELIMINARY RESULTS FOR TAU 8 9
10 /5/4 Constant Tau Nmin Nmin 3 Nmin 5 Nmin Mmin 2. Mmin 3. Mmin 4. Mmin Tau.5 Tau Nmin 3 5 Nb Eqks Mmin 2.: 65 eqks Mmin 3.: 56 eqks Mmin 4.: 26 eqks Mmin 5.: 6 eqks 9 Constant Tau: PIE/Tectonic.9.8 Nmin 5 All Eqks Tectonic Only PIE Only.9.8 Nmin 5, Mmin 3. All Eqks Tectonic Only PIE Only Tau.5 Tau At T. sec, All Eqks: 65 Tectonic Eqks: 54 PIE: At T. sec, All Eqks: 56 Tectonic Eqks: 45 PIE: 2
11 /5/4 Constant Tau: Comparisons Tau Mmin 3. CENA - Tectonic Only Zhao6 BSSA4 - M 4. CB4 - M 4. CY4 - M 4. ASK4 - M M- Dependent Tau and Comparisons T.sec CENA - Tectonic Only Zhao6 BSSA4 CB4 CY4 ASK Tsec CENA - Tectonic Only Zhao6 BSSA4 CB4 CY4 ASK4 Tau.5 Tau
12 /5/4 Depth- Dependence of Tau.9 T.sec All Eqks Tectonic Only.9 Tsec All Eqks Tectonic Only Tau.5 Tau Hypo Depth (km) Hypo Depth (km) 23 PRELIMINARY RESULTS FOR PHI 24 2
13 /5/4 Constant.9.8 Nmin 5, Mmin 3. All Eqks Tectonic Only PIE Only.9.8 Mmin Region 2, All Eqks.3 Region 2, Tectonic Only Region 2, PIE Only.2 Region 5. Region 3 Region 4.. At T. sec: All Eqks: 3,749 recs Tectonic:,9 recs PIE:,849 recs 25 Constant Comparisons Mmin 3. Mmin3 - Mmax6 - Rmax CENA - Tectonic Only CENA - PIE Only.3 Zhao6 BSSA4 - M4. - R3 - Vs76.2 CB4 - M4. - Vs76. CY4 - M4. - Vs76 meas ASK4 - M4. - Vs76 meas CENA - Tectonic Only.3 CENA - PIE Only ASK4.2 CB4. CY4 BSSA4.. Comparisons with proposed models Comparisons with NGA- W2 computed using within- event residuals 26 3
14 /5/4 M- Dependent and Comparisons T. sec T.sec T.sec - Rmax35km CENA - Tectonic CENA - PIE ASK4.2 CB4 CY4 BSSA4 27 M- Dependent and Comparisons T. sec Tsec Tsec - Rmax35km CENA - Tectonic CENA - PIE ASK4.2 CB4 CY4 BSSA4 28 4
15 /5/4 R- Dependent - T. sec T.sec T.sec - Mmin3 - Mmax6 CENA - Tectonic Only CENA - PIE Only Rrup (km).6.4 CENA - Tectonic Only CENA - PIE Only ASK4.2 CB4 CY4 BSSA Rrup (km) 29 R- Dependent - T. sec Tsec Tsec - Mmin3 - Mmax6 CENA - Tectonic Only CENA - PIE Only Rrup (km).6.4 CENA - Tectonic Only CENA - PIE Only ASK4.2 CB4 CY4 BSSA Rrup (km) 3 5
16 /5/4 MR- Dependent T. sec T.sec - M3 to4 T.sec - M4 to CENA - Tectonic Only.4 CENA - Tectonic Only.3 CENA - PIE Only.3 CENA - PIE Only.2 ASK4 CB4.2 ASK4 CB4. CY4 BSSA4. CY4 BSSA Rrup (km) Rrup (km) T.sec - M5 to CENA - Tectonic Only CENA - PIE Only ASK4 CB4 CY4 BSSA Rrup (km) 3 MR- Dependent T. sec Tsec - M3 to4 Tsec - M4 to CENA - Tectonic Only.4 CENA - Tectonic Only.3 CENA - PIE Only.3 CENA - PIE Only.2 ASK4 CB4.2 ASK4 CB4. CY4 BSSA4. CY4 BSSA Rrup (km) Rrup (km) Tsec - M5 to CENA - Tectonic Only CENA - PIE Only ASK4 CB4 CY4 BSSA Rrup (km) 32 6
17 /5/4 V S3 - Dependence of T.sec Tsec CENA - Tectonic Only CENA - PIE Only CENA - Tectonic Only CENA - PIE Only Vs3 (m/sec) Vs3 (m/sec) 33 PRELIMINARY RESULTS FOR PHISS 34 7
18 /5/4 Data DistribuIon at T. sec Min of 5 recs/eqk and 5 recs/sta: 3,33 recs (,632 Tect -,4 PIE) 65 eqks ( PIE) 337 staions 35 and Nmin = 5 recs S2S
19 /5/4 Constant Nmin 5 and Mmin 3. All Eqks Tectonic Only PIE Only Nmin = 5 and Mmin = 3. Region 2: All Eqks Region 2: Tectonic Only Region 2: PIE Only Region 5 Region At T. sec: All Eqks: 2,869 recs Tectonic:,468 recs PIE:,4 recs 37 Constant Comparisons Mmin3 - Mmax6 - Rmax35km CENA - Tectonic CENA - PIE ASK
20 /5/4 M- Dependent Comparisons T. sec Per. sec - Rmax km CENA - Tectonic Only CENA - PIE Only Per.- Rmax35km CENA - Tectonic CENA - PIE ASK M- Dependent Comparisons T. sec Per. sec - Rmax km CENA - Tectonic Only CENA - PIE Only Per.- Rmax35km CENA - Tectonic CENA - PIE ASK
21 /5/4 R- Dependent and Comparisons T. sec.2.8 Per.- M3 to6 CENA - Tectonic CENA - PIE ASK4.2.8 Per.- M3 to5 CENA - Tectonic CENA - PIE ASK Distance (km) Distance (km) 4 R- Dependent and Comparisons T. sec.2.8 Per.- M3 to6 CENA - Tectonic CENA - PIE ASK4.2.8 Per.- M3 to5 CENA - Tectonic CENA - PIE ASK Distance (km) Distance (km) 42 2
22 /5/4 MR- Dependent Comparisons Per.- M3 to4 CENA - Tectonic CENA - PIE ASK4 Euro T. sec Per.- M4 to5 CENA - Tectonic CENA - PIE ASK4 Taiw Euro Distance (km) Per.- M5 to Distance (km) CENA - Tectonic CENA - PIE ASK4 Taiw Euro Distance (km) 43 MR- Dependent Comparisons Per.- M3 to4 CENA - Tectonic CENA - PIE ASK4 Euro T. sec Per.- M4 to5 CENA - Tectonic CENA - PIE ASK4 Taiw Euro Distance (km) Per.- M5 to Distance (km) CENA - Tectonic CENA - PIE ASK4 Taiw Euro Distance (km) 44 22
23 /5/4 EvaluaIon of Path Effects for PIE Closeness index (CI) is used as an indicator of path similariies CI i, j, k = ( R + R ) 2 i, k ΔH i, j j, k H i,j = distance between the hypocenters of eqk i and j recorded at site s R i,k and R j,k = hypocentral distances from site k to eqk i and j. CI ranges from for co- located eqks to 2 for eqks located in opposite epicentral direcfons from the site 45 Path Effects for PIE: Closeness Index Calculate expected CI for randomly located earthquakes Calculate average CI for PIE Compare average CI for PIE to expected CI for randomly located earthquakes 46 23
24 /5/4 Expected CI for Randomly Located Eqks. Generate a number of randomly located earthquakes (Nhyp) in a circular area of radius R around a staion 2. Calculate CI for each pair of earthquakes at the staion 3. Calculate mean CI 4. Vary Nhypo and R Expected CI for randomly located earthquakes Closeness Index Region 2 δws Δ = i, j, k ik δws 2ϕ ss jk Region2 - T. Tectonic - Avg CI :.4 PIE - Avg CI :.55 Δ Closeness index, CI CI i, j, k = ( R + R ) 2 i, k ΔH i, j j, k Expected CI for randomly located earthquakes
25 /5/4 Closeness Index Region 3 and Region3 - T. Avg CI Region5 - T. Avg CI Δ Δ Closeness index, CI Closeness index, CI δws Δ = i, j, k ik δws 2ϕ ss jk CI i, j, k = ( R + R ) 2 i, k ΔH i, j j, k 49 Closeness Index; All Data Binned.4 T..4 T σ Δ σ Δ Lin et al. (2) CI for randomly located earthquakes:.38.2 Mean CI from data:.4 Data Closeness index, CI.4 Lin et al. (2) CI for randomly located earthquakes:.38.2 Mean CI from data:.98 Data Closeness index, CI σ Δ = mean 2 ( Δ ) At CI = à à At CI = 2 à à ss 2 ( ) ( ( 2 2 )) δ = Var δws δws E δws δws φ ρ δp P δp P φ 2 = = ijk ik jk ik jk P2P ik jk 5 25
26 /5/4 CANDIDATE MODELS FOR CENA: - New preliminary candidate models for Tau,, and - Exis-ng models for Tau,,, and ergodic Sigma 5 Proposed Tau Models Preliminary new models derived using tectonic CENA data Constant (M- independent) CENA model Period- dependence M- dependent CENA model: ExtrapolaIon beyond M4.5 ExisIng Tau models: EPRI 23: M- dependent based on avg of preliminary 4 NGA- W2 Tau values; Increased by
27 /5/4 Constant CENA Tau Model.9.8 CENA - Mmin 3. CENA - Mmin Tau Used data with Mmin 3. to derive Tau model (45 versus 2 earthquakes) 53 Constant CENA Tau Model (cont d) CENA Zhao6 BSSA4 - M 4. CB4 - M 4. CY4 - M 4. ASK4 - M 4. Tau
28 /5/4 M- Dependent CENA Tau Model T.sec CENA BSSA4 CB4 CY4 ASK T.sec CENA BSSA4 CB4 CY4 ASK4.6.6 Tau.5 Tau For M < 4.5; Tau is mean of values for M 3. to 4.5 bins 2 opions for M > 4.5 extrapolaion: Same slope as CB4 Tau from M 4.5 to 5.5 Tau reaches the same CB4 Tau for M >= M- Dependent CENA Tau Model (cont d) T.5sec CENA BSSA4 CB4 CY4 ASK Tsec CENA BSSA4 CB4 CY4 ASK4.6.6 Tau.5 Tau For M < 4.5; Tau is mean of values for M 3. to 4.5 bins 2 opions for M > 4.5 extrapolaion: Same slope as CB4 Tau from M 4.5 to 5.5 Tau reaches the same CB4 Tau for M >=
29 /5/4 EPRI 23 Tau Model.9.8 EPRI 23 - M5 EPRI 23 - M6 EPRI 23 - M7.7.6 Tau Comparison of Candidate Tau Models Tau
30 /5/4 Proposed Models Preliminary models derived using tectonic data with distances less than 4 km values affected by site classificaion issues Two new derived models: Constant M- dependent and issue of extrapolaion to large M ExisIng models: EPRI 23: M- dependent based on avg of preliminary 4 NGA- W2 values 59 Constant CENA Model.8 Mmin 3. Rmax :,9 recs Mmin 3. Rmax 4: 65 recs Mmin 4. Rmax : 727 recs Mmin 4. Rmax 4: 25 recs.6.4 Mmin 3. - Rmax.2 Mmin 3. - Rmax 4 Mmin 4. - Rmax Mmin 4. - Rmax 4.. Used data with Mmin 3. and Rmax 4 km to derive model 6 3
31 /5/4 Constant CENA Model (cont d) CENA BSSA4 - M4. - R25 - Vs76.2 CB4 - M4. - Vs76. CY4 - M4. - Vs76 meas ASK4 - M4. - Vs76 meas.. 6 M- Dependent CENA Model T.sec T.sec CENA - Rmax 4 BSSA4 - R25 - Vs76.2 CB4 - Vs76 CY4 - Vs76 meas ASK4 - Vs76 meas.4 CENA - Rmax 4 BSSA4 - R25 - Vs76.2 CB4 - Vs76 CY4 - Vs76 meas ASK4 - Vs76 meas For M < 4.5; is mean of values for M 3. to 4.5 bins 2 opions for M > 4.5 extrapolaion: Same slope as BSSA4 from M 4.5 to 5.5 reaches the same BSSA4 for M >=
32 /5/4 M- Dependent CENA Model (cont d) T.5sec Tsec CENA - Rmax 4 BSSA4 - R25 - Vs76.2 CB4 - Vs76 CY4 - Vs76 meas ASK4 - Vs76 meas.4 CENA - Rmax 4 BSSA4 - R25 - Vs76.2 CB4 - Vs76 CY4 - Vs76 meas ASK4 - Vs76 meas For M < 4.5; is mean of values for M 3. to 4.5 bins 2 opions for M > 4.5 extrapolaion: Same slope as BSSA4 from M 4.5 to 5.5 reaches the same BSSA4 for M >= EPRI 23 Model EPRI 23 - M 5. EPRI 23 - M 6 EPRI 23 - M
33 /5/4 Comparison of Candidate Models EPRI 23 - M 5.4 EPRI 23 - M 6 EPRI 23 - M 7.3 New - Constant New - MDep - M5 - Option.2 New - MDep - M5 - Option 2. New - MDep - M > Option New - MDep - M> Option ExisIng Ergodic Sigma Models EPRI 23: and Tau are based on NGA- West2 standard deviaions Atkinson and Adams 23: NaIonal seismic hazard maps of Canada Atkinson and Boore 26 Toro et al
34 /5/4 ExisIng Ergodic Sigma Models 67 Proposed Models Preliminary models derived using tectonic data with distances less than 4 km Two new derived models: Constant; M- dependent ExisIng models: Constant: PRP SWUS Project Italian Model (Luzi et al. 24) M- dependent: Thyspunt Project South Africa Hanford Project SWUS Project R- dependent: PRP MR- dependent: PRP 68 34
35 /5/4 Overview of ExisIng Models PRP: Global dataset (CA, Switzerland, Taiwan, Turkey, Japan), M >= 4.5, Rrup <= 2 km No regional dependence of Models: constant, R- dependent, MR- dependent Thyspunt Project and Hanford Project: Global dataset; PRP dataset M- dependent model 69 Overview of ExisIng Models (cont d) SWUS Project: DCPP: NGA- W2 data with M >= 5. and Rrup < 5 km 2 constant models (CA only and global) M- dependent model (CA only) PVNGS: Distant sources: constant model for M >= 5.5 and R = 2 to 4 km; NGA- W2 dataset Local sources: 2 constant models (NGA- W2 and Euro data of ASK3) with M >= 5. and Rrup < 5 km Luzi et al. (24): Italian data (3 sets) with M 4. to 7. and Rjb < 2 km Constant Models Others: BCHydro and Hanford Project for subducion earthquakes - Constant 7 35
36 /5/4 Constant CENA Model CENA - Mmin 3. - Rmax CENA - Mmin 3. - Rmax 4 CENA - Mmin 4. - Rmax CENA - Mmin 4. - Rmax 4 Mmin 3. Rmax :,468 recs Mmin 3. Rmax 4: 494 recs Mmin 4. Rmax : 53 recs Mmin 4. Rmax 4: 7 recs Used data with Mmin 3. and Rmax 4 km to derive model 7 Constant CENA Model (cont d).9.8 CENA - Mmin 3. - Rmax 4 ASK4 - Mmin 3. - Mmax 6. - Rmax
37 /5/4 ExisIng Constant Models CENA - Mmin 3. - Rmax 4 New Model PRP - Central PRP - Low PRP - High CENA - Mmin 3. - Rmax 4 New Model Italy, Italy, 2 Italy, PRP: Global data M >= 4.5, Rrup <= 2 km Italian data: M 4. to 7., RJB < 2 km 73 ExisIng Constant Models (cont d) DCPP CA (Blue): M >= 5.5, Rrup < 5 km DCPP Global (red): same M- R range PVNGS Distant Sources (Blue): M >= 5.5, Rrup 2 to 4 km PVNGS Short Distance European Data (red) M >= 5., Rrup < 5 km PVNGS Short Distance Global Data (green) 74 37
38 /5/4 M- dependent CENA Model Per. CENA - Rmax 4 ASK4 Model CENA Model ASK Per. CENA - Rmax 4 ASK4 Model CENA Model ASK M- dependent CENA Model (cont d) Per.5 CENA - Rmax 4 ASK4 Model CENA Model ASK Per. CENA - Rmax 4 ASK4 Model CENA Model ASK
39 /5/4 ExisIng M- dependent Models T. sec T. sec Hanford Model Black Global data; Rrup <= 2 km DCPP M- dependent Model Red CA NGA- W2 data; Rrup < 5 km 77 ExisIng R- dependent Model: PRP.9 Per. CENA - Mmin 4..9 Per. CENA - Mmin Distance (km) Distance (km) 78 39
40 /5/4 ExisIng MR- dependent Model: PRP Per.- M3 to4 Per.- M4 to Distance (km) Distance (km) Per.- M5 to6 Per.- M6 to Distance (km) Distance (km) 79 ExisIng MR- dependent Model: PRP Per.- M3 to4 Per.- M4 to Distance (km) Distance (km).8 Per.- M5 to6 CENA ASK4.8 Per.- M6 to Distance (km) Distance (km) 8 4
41 /5/4 Summary New CENA models suffer from biased dataset (small M, large distance) and potenial site classificaion issues Constant models may not be reasonable to apply for large M M- dependent models may do bemer Issue of extrapolaion to larger M 8 To Do New CENA models: Using residuals from a revised regression. Issue of site terms for Lowest useable period for TA data Q- specific for PIE data Use Nmin 3 and increase Rmax to maximize dataset. Incorporate PIE? More thorough evaluaion of exising models 82 4
42 /5/4 THANK YOU! 83 and S2S for Different Nmin Nmin Nmin3 Nmin5 Nmin Nmin Nmin3 Nmin5 Nmin S2S Nb of Recs Nb of Sta Nb of Eqks Nmin 3, Nmin 3 3, Nmin 5 3, Nmin,
43 /5/4 V s3 - Dependent and Comparisons Per.- M3 to6- Rmax35km Per.- M3 to6- Rmax35km CENA - Tectonic CENA - PIE ASK4 CENA - Tectonic CENA - PIE ASK Vs3 (m/sec) Vs3 (m/sec) 85 43
Single-Station Phi Using NGA-West2 Data
SSHAC Level 3 Southwestern U.S. Ground Motion Characterization WS-2, October 24, 23 Berkeley, CA Single-Station Phi Using NGA-West2 Data Linda Al Atik Proponent Expert Outline Background, terminology and
More informationAdrian Rodriguez Marek Virginia Tech
A Single Station Station Sigma Model Adrian Rodriguez Marek Virginia Tech with contributions from Fabrice Cotton, Norm Abrahamson, Sinan Akkar, Linda Al Atik, John Anderson, Fabian Bonilla, Julian Bommer,
More informationHazard Feedback using the. current GMPEs for DCPP. Nick Gregor. PG&E DCPP SSHAC Study. SWUS GMC Workshop 2 October 22, 2013
1 Hazard Feedback using the current GMPEs for DCPP Nick Gregor PG&E DCPP SSHAC Study SWUS GMC Workshop 2 October 22, 2013 PGA Hazard By Source 0.5 Hz 2 Deaggregation AEP = 10-4 PGA 0.5 Hz 3 4 Base Case
More informationGround Motion Prediction Equation Hazard Sensitivity Results for Palo Verde Nuclear Generating Station Site (PVNGS)
Ground Motion Prediction Equation Hazard Sensitivity Results for Palo Verde Nuclear Generating Station Site (PVNGS) M.Walling SWUS GMC Workshop 3 March 11, 2013 Hazard ground motion prediction equation
More informationSELECTION OF GROUND-MOTION PREDICTION EQUATIONS FOR PROBABILISTIC SEISMIC HAZARD ANALYSIS : CASE STUDY OF TAIWAN
5 th IASPEI / IAEE International Symposium Effects of Surface Geology on Seismic Motion SELECTION OF GROUND-MOTION PREDICTION EQUATIONS FOR PROBABILISTIC SEISMIC HAZARD ANALYSIS : CASE STUDY OF TAIWAN
More informationNon-Ergodic Probabilistic Seismic Hazard Analyses
Non-Ergodic Probabilistic Seismic Hazard Analyses M.A. Walling Lettis Consultants International, INC N.A. Abrahamson University of California, Berkeley SUMMARY A method is developed that relaxes the ergodic
More informationGMPEs for Active Crustal Regions: Applicability for Controlling Sources
GMPEs for Active Crustal Regions: Applicability for Controlling Sources Jonathan P. Stewart University of California, Los Angeles March 19, 2013 Oakland Airport Hilton Outline GMPEs considered GMPE parameter
More informationNGA-Subduction: Development of the Largest Ground Motion Database for Subduction Events
NGA-Subduction: Development of the Largest Ground Motion Database for Subduction Events Tadahiro Kishida. Ph.D., and Yousef Bozorgnia, Ph.D., P.E. University of California, Berkeley 1 Probabilistic Seismic
More informationNext Generation Attenuation (NGA) Projects
Next Generation Attenuation (NGA) Projects Yousef Bozorgnia, Ph.D., P.E. Executive Director, Pacific Earthquake Engineering Research Center (PEER), University of California, Berkeley NGA= Next Generation
More informationKappa for Candidate GMPEs
SSHAC Level 3 Southwestern U.S. Ground Motion Characterization WS-1, March 21, 2013 Oakland, CA Kappa for Candidate GMPEs Linda Al Atik Resource Expert Overview Kappa controls the highfrequency spectral
More informationUpdating the Chiou and YoungsNGAModel: Regionalization of Anelastic Attenuation
Updating the Chiou and YoungsNGAModel: Regionalization of Anelastic Attenuation B. Chiou California Department of Transportation R.R. Youngs AMEC Environment & Infrastructure SUMMARY: (10 pt) Ground motion
More informationNon-Ergodic Site Response in Seismic Hazard Analysis
Non-Ergodic Site Response in Seismic Hazard Analysis Jonathan P. Stewart, Ph.D., P.E. Professor and Chair Civil & Environmental Engineering Dept. University of California, Los Angeles ESG 5 Taipei, Taiwan
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER NGA-East Ground-Motion Models for the U.S. Geological Survey National Seismic Hazard Maps Christine A. Goulet Yousef Bozorgnia Nicolas Kuehn Pacifi c Earthquake
More informationBSSA12 GMPEs. Dave Boore, Jon Stewart, Emel Seyhan, Gail Atkinson. NGA- West2 Public MeeCng Berkeley, California 15 November 2012
BSSA12 GMPEs Dave Boore, Jon Stewart, Emel Seyhan, Gail Atkinson NGA- West2 Public MeeCng Berkeley, California 15 November 2012 1 Model DescripCon BA08 funcconal form for M and R jb scaling Change from
More informationGround-Motion Prediction Equations (GMPEs) from a Global Dataset: The PEER NGA Equations
Ground-Motion Prediction Equations (GMPEs) from a Global Dataset: The PEER NGA Equations David M. Boore U.S. Geological Survey Abstract The PEER NGA ground-motion prediction equations (GMPEs) were derived
More informationInsights on stress- drop magnitude- dependency and variability from the analysis of accelerometric data.
Insights on stress- drop magnitude- dependency and variability from the analysis of accelerometric data. Fabrice Co+on - GFZ German Research Centre for Geosciences, Potsdam Boumediene Derras - ISTerre,
More informationPEER RVT approach: Duration Model
PEER RVT approach: Duration Model Nicolas Kuehn Norm Abrahamson, Christine Goulet, Justin Hollenback Pacific Earthquake Engineering Research Center NGA East Workshop 30 October 2014 Motivation To calculate
More informationRECORD OF REVISIONS. Page 2 of 17 GEO. DCPP.TR.14.06, Rev. 0
Page 2 of 17 RECORD OF REVISIONS Rev. No. Reason for Revision Revision Date 0 Initial Report - this work is being tracked under Notification SAPN 50638425-1 8/6/2014 Page 3 of 17 TABLE OF CONTENTS Page
More informationGround Motion Prediction Equations: Past, Present, and Future
Ground Motion Prediction Equations: Past, Present, and Future The 2014 William B. Joyner Lecture David M. Boore As presented at the SMIP15 meeting, Davis, California, 22 October 2015 The William B. Joyner
More informationDIRECT HAZARD ANALYSIS OF INELASTIC RESPONSE SPECTRA
DIRECT HAZARD ANALYSIS OF INELASTIC RESPONSE SPECTRA ABSTRACT Y. Bozorgnia, M. Hachem, and K.W. Campbell Associate Director, PEER, University of California, Berkeley, California, USA Senior Associate,
More informationComparison of NGA-West2 GMPEs
Comparison of NGA-West2 GMPEs Nick Gregor, a) M.EERI, Norman A. Arahamson, ) M.EERI, Gail M. Atkinson, c) M.EERI, David M. Boore, d) Yousef Bozorgnia, e) M.EERI, Kenneth W. Campell, f) M.EERI, Brian S.-J.
More informationUpdated NGA-West2 Ground Motion Prediction Equations for Active Tectonic Regions Worldwide
Updated NGA-West2 Ground Motion Prediction Equations for Active Tectonic Regions Worldwide Kenneth W. Campbell 1 and Yousef Bozorgnia 2 1. Corresponding Author. Vice President, EQECAT, Inc., 1130 NW 161st
More informationSpatial Cross-correlation Models for Vector Intensity Measures (PGA, Ia, PGV and Sa s) Considering Regional Site Conditions
Spatial Cross-correlation Models for Vector Intensity Measures (PGA, Ia, PGV and Sa s) Considering Regional Site Conditions Gang Wang and Wenqi Du Department of Civil and Environmental Engineering Hong
More informationVertical to Horizontal (V/H) Ratios for Large Megathrust Subduction Zone Earthquakes
Vertical to Horizontal (V/H) Ratios for Large Megathrust Subduction Zone Earthquakes N.J. Gregor Consultant, Oakland, California, USA N.A. Abrahamson University of California, Berkeley, USA K.O. Addo BC
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER. NGA-West2 Ground Motion Prediction Equations for Vertical Ground Motions
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER NGA-West2 Ground Motion Prediction Equations for Vertical Ground Motions PEER 2013/24 SEPTEMBER 2013 Disclaimer The opinions, findings, and conclusions or
More informationRecent Advances in Development of Ground Motion Prediction Equations
Recent Advances in Development of Ground Motion Prediction Equations Yousef Bozorgnia, Ph.D., P.E. Executive Director, Pacific Earthquake Engineering Research Center (PEER), University of California, Berkeley
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER Update of the AS08 Ground-Motion Prediction Equations Based on the NGA-West2 Data Set Norman A. Abrahamson Pacific Gas & Electric Company San Francisco, California
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER Update of the BC Hydro Subduction Ground-Motion Model using the NGA-Subduction Dataset Norman Abrahamson Nicolas Kuehn University of California, Berkeley
More informationDEVELOPING TIME HISTORIES WITH ACCEPTABLE RECORD PARAMETERS FOR DILLON DAM. Dina Bourliea Hunt, P.E. 1 Justin Beutel, P.E. 2 Christine Weber, P.E.
DEVELOPING TIME HISTORIES WITH ACCEPTABLE RECORD PARAMETERS FOR DILLON DAM Dina Bourliea Hunt, P.E. 1 Justin Beutel, P.E. 2 Christine Weber, P.E. 3 ABSTRACT Dillon Dam project is located in Summit County,
More informationUpdated Graizer-Kalkan GMPEs (GK13) Southwestern U.S. Ground Motion Characterization SSHAC Level 3 Workshop 2 Berkeley, CA October 23, 2013
Updated Graizer-Kalkan GMPEs (GK13) Southwestern U.S. Ground Motion Characterization SSHAC Level 3 Workshop 2 Berkeley, CA October 23, 2013 PGA Model Our model is based on representation of attenuation
More informationGlobal Earthquake Model. KICK-OFF MEETING PEER UC Berkeley 16 th February Global Components - Hazard Ground Motion Prediction Equations (GMPEs)
Global Earthquake Model Global Components - Hazard Ground Motion Prediction Equations (GMPEs) KICK-OFF MEETING PEER UC Berkeley 16 th February 2011 Carola Di Alessandro and Yousef Bozorgnia GMPEs Consortium
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER Identification of Site Parameters that Improve Predictions of Site Amplification Ellen M. Rathje Sara Navidi Department of Civil, Architectural, and Environmental
More informationEstimation of Strong Ground Motion: Aleatory Variability and Epistemic Uncertainty
Estimation of Strong Ground Motion: Aleatory Variability and Epistemic Uncertainty 5th National Conference on Earthquake Engineering 1st National Conference on Earthquake Engineering and Seismology Bucharest,
More informationA Local Ground-Motion Predictive Model for Turkey, and Its Comparison with Other Regional and Global Ground-Motion Models
Bulletin of the Seismological Society of America, Vol. 1, No. 6, pp. 978 995, December 1, doi: 1.1785/19367 A Local Ground-Motion Predictive Model for Turkey, and Its Comparison with Other Regional and
More informationVALIDATION AGAINST NGA EMPIRICAL MODEL OF SIMULATED MOTIONS FOR M7.8 RUPTURE OF SAN ANDREAS FAULT
VALIDATION AGAINST NGA EMPIRICAL MODEL OF SIMULATED MOTIONS FOR M7.8 RUPTURE OF SAN ANDREAS FAULT L.M. Star 1, J. P. Stewart 1, R.W. Graves 2 and K.W. Hudnut 3 1 Department of Civil and Environmental Engineering,
More informationComparisons of ground motions from the M 9 Tohoku earthquake with ground-motion prediction equations for subduction interface earthquakes
Comparisons of ground motions from the M 9 Tohoku earthquake with ground-motion prediction equations for subduction interface earthquakes David M. Boore 8 March 20 Revised: 3 March 20 I used data from
More informationAre Ground-Motion Models Derived from Natural Events Applicable to the Estimation of Expected Motions for Induced Earthquakes?
Are Ground-Motion Models Derived from Natural Events Applicable to the Estimation of Expected Motions for Induced Earthquakes? by Gail M. Atkinson and Karen Assatourians ABSTRACT Natural earthquakes in
More informationGround Motion Prediction Equations for Application to the 2015 Canadian National Seismic Hazard Maps
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 Ground Motion Prediction Equations for Application to the 2015 Canadian National Seismic Hazard Maps Can. J. Civ. Eng.
More informationSCEC Broadband Platform (BBP) Simulation Methods Validation for NGA-East
SCEC Broadband Platform (BBP) Simulation Methods Validation for NGA-East BBP Validation Team: N. Abrahamson, P. Somerville, F. Silva, P. Maechling, R. Archuleta, J. Anderson, K. Assatourians, G. Atkinson,
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER Semi-Empirical Nonlinear Site Amplification and its Application in NEHRP Site Factors Jonathan P. Stewart Emel Seyhan Department of Civil and Environmental
More informationThe Role of Physics-Based Ground Motion Models in Non-Ergodic Site-Specific PSHA Studies
The Role of Physics-Based Ground Motion Models in Non-Ergodic Site-Specific PSHA Studies Luis A. Dalguer and Philippe Renault Hazard and Structural Analysis Swissnuclear, Switzerland Disclaimer: This presentation
More informationBulletin of the Seismological Society of America
Bulletin of the Seismological Society of America This copy is for distribution only by the authors of the article and their institutions in accordance with the Open Access Policy of the Seismological Society
More informationIntroduction to Strong Motion Seismology. Norm Abrahamson Pacific Gas & Electric Company SSA/EERI Tutorial 4/21/06
Introduction to Strong Motion Seismology Norm Abrahamson Pacific Gas & Electric Company SSA/EERI Tutorial 4/21/06 Probabilistic Methods Deterministic Approach Select a small number of individual earthquake
More informationCALIBRATING THE BACKBONE APPROACH FOR THE DEVELOPMENT OF EARTHQUAKE GROUND MOTION MODELS
1 Best Practices in Physics-based Fault Rupture Models for Seismic Hazard Assessment of Nuclear CALIBRATING THE BACKBONE APPROACH FOR THE DEVELOPMENT OF EARTHQUAKE GROUND MOTION MODELS J. DOUGLAS 1 1 University
More informationEpistemic Uncertainty: Previous Approaches
Epistemic Uncertainty: Previous Approaches N. Abrahamson NGA- East workshop Jul 14, 214 Epistemic Uncertainty: Discrete RepresentaFon of ConFnuous DistribuFon Logic Trees for Ground MoFons Examples of
More informationby Shahram Pezeshk, Arash Zandieh, Kenneth W. Campbell, and Behrooz Tavakoli Introduction
Bulletin of the Seismological Society of America, Vol. 108, No. 4, pp. 2278 2304, August 2018, doi: 10.1785/0120170179 Ground-Motion Prediction Equations for Central and Eastern North America Using the
More informationNGA-West 2 Equations for Predicting PGA, PGV, and 5%-Damped PSA for Shallow Crustal Earthquakes
NGA-West 2 Equations for Predicting PGA, PGV, and 5%-Damped PSA for Shallow Crustal Earthquakes David M. Boore, a) Jonathan P. Stewart, b) M.EERI, Emel Seyhan, b) M.EERI, and Gail M. Atkinson, (c) M.EERI
More informationUPDATED PROBABILISTIC SEISMIC HAZARD MAPS FOR TURKEY
UPDATED PROBABILISTIC SEISMIC HAZARD MAPS FOR TURKEY S. Akkar, T. Azak, T. Çan, U. Çeken, M.B. Demircioğlu, T.Y. Duman, M. Erdik, S. Ergintav, F.T. Kadirioğlu, D. Kalafat, Ö. Kale, R.F. Kartal, K. Kekovalı,
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER Update of the BC Hydro Subduction Ground-Motion Model using the NGA-Subduction Dataset Norman Abrahamson Nicolas Kuehn University of California, Berkeley
More informationAn NGA Model for the Average Horizontal Component of Peak Ground Motion and Response Spectra
An NGA Model for the Average Horizontal Component of Peak Ground Motion and Response Spectra Brian S.-J. Chiou a) and Robert R. Youngs, b) M.EERI We present a model for estimating horizontal ground motion
More informationProposed Approach to CENA Site Amplification
Proposed Approach to CENA Site Amplification Gail Atkinson with acknowledgement to many co-authors, especially Ghofrani, Hassani, Assatourians, and Braganza. The model is a team effort reflecting their
More informationBeyond Sa GMRotI : Conversion to Sa Arb, Sa SN, and Sa MaxRot
Bulletin of the Seismological Society of America, Vol. 97, No. 5, pp. 1511 1524, October 2007, doi: 10.1785/0120070007 Beyond Sa GMRotI : Conversion to Sa Arb, Sa SN, and Sa MaxRot by Jennie A. Watson-Lamprey
More informationJulian J Bommer, Peter J Stafford & Michail Ntinalexis. Datum November Jan van Elk & Dirk Doornhof
Empirical Ground-Motion Prediction Equations for Peak Ground Velocity from Small-Magnitude Earthquakes in the Groningen Field Using Multiple Definitions of the Horizontal Component of Motion Updated Model
More informationSeismic hazard modeling for Bulgaria D. Solakov, S. Simeonova
Seismic hazard modeling for Bulgaria D. Solakov, S. Simeonova Bulgarian seismic network and foreign stations used in epicenter location Sismicity in Bulgaria and surroundings (M 4.) Epicentral map for
More informationEmpirical Correlations between Cumulative Absolute Velocity and Amplitude-Based Ground Motion Intensity Measures
Empirical Correlations between Cumulative Absolute Velocity and Amplitude-Based Ground Motion Intensity Measures Brendon A Bradley a) b) Empirical correlation equations are developed between cumulative
More informationL. Danciu, D. Giardini, J. Wößner Swiss Seismological Service ETH-Zurich Switzerland
BUILDING CAPACITIES FOR ELABORATION OF NDPs AND NAs OF THE EUROCODES IN THE BALKAN REGION Experience on the field of seismic hazard zonation SHARE Project L. Danciu, D. Giardini, J. Wößner Swiss Seismological
More informationCAMPBELL-BOZORGNIA NEXT GENERATION ATTENUATION (NGA) RELATIONS FOR PGA, PGV AND SPECTRAL ACCELERATION: A PROGRESS REPORT
Proceedings of the 8 th U.S. National Conference on Earthquake Engineering April 18-22, 2006, San Francisco, California, USA Paper No. 906 CAMPBELL-BOZORGNIA NEXT GENERATION ATTENUATION (NGA) RELATIONS
More informationGEM-PEER Global GMPEs Project Guidance for Including Near-Fault Effects in Ground Motion Prediction Models
GEM-PEER Global GMPEs Project Guidance for Including Near-Fault Effects in Ground Motion Prediction Models J.W. Baker Stanford University, Stanford, CA, USA Y. Bozorgnia & C. Di Alessandro PEER Center,
More informationRupture directivity effects during the April 15, 2016 Kumamoto. Mw7.0 earthquake in Japan
Rupture directivity effects during the April 15, 16 Kumamoto Mw7. earthquake in Japan Junju Xie 1, Paolo Zimmaro, Xiaojun Li 1*, Zengping Wen 1 1 Institute of Geophysics, China Earthquake Administration,
More informationAn evaluation of the applicability of the NGA models to ground-motion prediction in the Euro-Mediterranean region
Bull Earthquake Eng (28) 6:49 77 DOI 7/s58-7-953-2 ORIGINAL RESEARCH PAPER An evaluation of the applicability of the NGA models to ground-motion prediction in the Euro-Mediterranean region Peter J. Stafford
More informationA Test of the Applicability of NGA Models to the Strong Ground-Motion Data in the Iranian Plateau
Journal of Earthquake Engineering, 14:278 292, 2010 Copyright Ó A.S. Elnashai & N.N. Ambraseys ISSN: 1363-2469 print / 1559-808X online DOI: 10.1080/13632460903086051 A Test of the Applicability of NGA
More informationRepeatable Source, Site, and Path Effects on the Standard Deviation for Empirical Ground-Motion Prediction Models
Bulletin of the Seismological Society of America, Vol., No. 5, pp. 8 95, October, doi:.785/93 Repeatable Source, Site, and Path Effects on the Standard Deviation for Empirical Ground-Motion Prediction
More informationSelection of a Global Set of GMPEs for the GEM-PEER Global GMPEs Project
Selection of a Global Set of GMPEs for the GEM-PEER Global GMPEs Project J.P. Stewart University of California, Los Angeles, USA J. Douglas BRGM, Orleans, France C. Di Alessandro, Y. Bozorgnia, and N.A.
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER NGA-West2 Campbell-Bozorgnia Ground Motion Model for the Horizontal Components of PGA, PGV, and 5%-Damped Elastic Pseudo-Acceleration Response Spectra for
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER NGA-West2 Equations for Predicting Response Spectral Accelerations for Shallow Crustal Earthquakes David M. Boore US Geological Survey Menlo Park, CA Jonathan
More informationDirectivity in NGA Earthquake Ground Motions: Analysis Using Isochrone Theory
Directivity in NGA Earthquake Ground Motions: Analysis Using Isochrone Theory Paul Spudich, a) M.EERI, and Brian S. J. Chiou b) We present correction factors that may be applied to the ground motion prediction
More informationNGA-West2 Equations for Predicting Vertical-Component PGA, PGV, and 5%-Damped PSA from Shallow Crustal Earthquakes
NGA-West2 Equations for Predicting Vertical-Component PGA, PGV, and 5%-Damped PSA from Shallow Crustal Earthquakes Jonathan P. Stewart, a) M.EERI, David M. Boore, b) Emel Seyhan, c) M.EERI, and Gail M.
More informationNGA-West2 Research Project
NGA-West2 Research Project Yousef Bozorgnia, a) M.EERI, Norman A. Abrahamson, b) M.EERI, Linda Al Atik, c) M.EERI, Timothy D. Ancheta, d) M.EERI, Gail M. Atkinson, e) M.EERI, Jack W. Baker, f) M.EERI,
More informationKenneth W. Campbell EQECAT, Inc. Beaverton, Oregon. Yousef Bozorgnia Pacific Earthquake Engineering Research Center University of California, Berkeley
Campbell-Bozorgnia NGA Empirical Ground Motion Model for the Average Horizontal Component of PGA, PGV, PGD and SA at Selected Spectral Periods Ranging from 0.01 10.0 Seconds (Version 1.1) Kenneth W. Campbell
More informationKenneth W. Campbell EQECAT, Inc. Beaverton, Oregon. Yousef Bozorgnia Pacific Earthquake Engineering Research Center University of California, Berkeley
Campbell-Bozorgnia NGA Empirical Ground Motion Model for the Average Horizontal Component of PGA, PGV, PGD and SA at Selected Spectral Periods Ranging from 0.01 10.0 Seconds (Version 1.0) Kenneth W. Campbell
More informationIntra-Event Spatial Correlations for Cumulative Absolute Velocity, Arias Intensity, and Spectral Accelerations Based on Regional Site Conditions
Bulletin of the Seismological Society of America, Vol. 103, No. 2A, pp. 1117 1129, April 2013, doi: 10.1785/0120120185 Intra-Event Spatial Correlations for Cumulative Absolute Velocity, Arias Intensity,
More informationPEER PSHA Code Verification Project. Christie Hale Norm Abrahamson Yousef Bozorgnia
PEER PSHA Code Verification Project Christie Hale Norm Abrahamson Yousef Bozorgnia Agenda Introduction and Approach Details on Three Tests Which codes completed which tests? Probabilistic Seismic Hazard
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER NGA Model for Average Horizontal Component of Peak Ground Motion and Response Spectra Brian S.-J. Chiou California Department of Transportation and Robert
More informationNGA-East Station Database Draft Site Metadata: V S30
NGA-East Station Database Draft Site Metadata: V S30 Youssef. M. A. Hashash, Joseph Harmon, Jonathan P. Stewart, Albert Kottke, Byungmin Kim, Walt Silva, Ellen Rathje, Kenneth W. Campbell 14 July 2014
More informationSeismic Vulnerability Assessment of Wood-frame Buildings in Southwestern British Columbia
Seismic Vulnerability Assessment of Wood-frame Buildings in Southwestern British Columbia K. Goda University of Bristol, United Kingdom G.M. Atkinson University of Western Ontario, Canada ABSTRACT: The
More informationPACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER NGA-West2 Models for Ground-Motion Directionality Shrey K. Shahi Jack W. Baker Department of Civil and Environmental Engineering Stanford University PEER
More informationHybrid Empirical Ground-Motion Prediction Equations for Eastern North America Using NGA Models and Updated Seismological Parameters
Hybrid Empirical Ground-Motion Prediction Equations for Eastern North America Using NGA Models and Updated Seismological Parameters by Shahram Pezeshk, 1 Arash Zandieh, 1 and Behrooz Tavakoli 2 1 Department
More informationDevelopment of Ground Motion Time Histories for Seismic Design
Proceedings of the Ninth Pacific Conference on Earthquake Engineering Building an Earthquake-Resilient Society 14-16 April, 2011, Auckland, New Zealand Development of Ground Motion Time Histories for Seismic
More informationSHARE-GEM hazard map released yesterday
SHARE-GEM hazard map released yesterday PGA 475 years D. Giardini, J. Woessner, L. Danciu, H. Crowley, F. Cotton, G. Gruenthal, R. Pinho, G. Valensise, S. Akkar, R. Arvidsson, R. Basili, T. Cameelbeck,
More informationZach Bullock Brendon A. Bradley. Research report Department of Civil Engineering University of Canterbury Christchurch New Zealand
SYSTEMATIC VERTICAL GROUND MOTION OBSERVATIONS IN THE CANTERBURY EARTHQUAKES Zach Bullock Brendon A. Bradley Research report 2016-03 Department of Civil Engineering University of Canterbury Christchurch
More informationSpatial Correlation of Ground Motions in Seismic Hazard Assessment
Spatial Correlation of Ground Motions in Seismic Hazard Assessment Taojun Liu tliu82@uwo.ca Department of Civil & Environmental Engineering University of Western Ontario London, Ontario, Canada 1 Outline
More informationGMPE Implementation in OpenQuake (and GEM s Development Tools) Graeme Weatherill
GMPE Implementation in OpenQuake (and GEM s Development Tools) Graeme Weatherill GMPEs in OpenQuake 1. Overview of OpenQuake Development 2. GMPE Testing and Quality Assurance 3. Source and Site Characterisation
More informationEleventh U.S. National Conference on Earthquake Engineering Integrating Science, Engineering & Policy June 25-29, 2018 Los Angeles, California
Eleventh U.S. National Conference on Earthquake Engineering Integrating Science, Engineering & Policy June 25-29, 2018 Los Angeles, California Site-Specific MCE R Response Spectra for Los Angeles Region
More informationModifications to Existing Ground-Motion Prediction Equations in Light of New Data
Bulletin of the Seismological Society of America, Vol. 101, No. 3, pp. 1121 1135, June 2011, doi: 10.1785/0120100270 Modifications to Existing Ground-Motion Prediction Equations in Light of New Data by
More informationHosgri Fault Location and Dip SSC TI Team Evaluation Hans AbramsonWard
1 Hosgri Fault Location and Dip SSC TI Team Evaluation Hans AbramsonWard PG&E DCPP SSHAC Study 2 Key Data Sources PE Models: Johnson WS2 presentation Hardebeck WS2 presentation Watt WS2 presentation AbramsonWard
More information25 July 2005: Dave s notes on work done for PEER NGA project File: \peer_nga\teamx\daves_notes_mechrake_c3_stage1_stage2_pga_25july2005.
25 July 2005: Dave s notes on work done for PEER NGA project File: \peer_nga\teamx\daves_notes_mechrake_c3_stage1_stage2_pga_25july2005.doc These notes cover 1) the choice of the mechanism determination
More informationThe effect of bounds on magnitude, source-to-site distance and site condition in PSHA-based ground motion selection
The effect of bounds on magnitude, source-to-site distance and site condition in PSHA-based ground motion selection K. Tarbali & B.A. Bradley Department of Civil and Natural Resources Engineering, University
More informationEmpirical Ground-Motion Models for Point- and Extended-Source Crustal Earthquake. Scenarios in Europe and the Middle East
Accepted for publication in Bulletin of Earthquake Engineering Empirical Ground-Motion Models for Point- and Extended-Source Crustal Earthquake Scenarios in Europe and the Middle East S. Akkar 1, M.A.
More informationHybrid Empirical Ground-Motion Prediction Equations for Eastern North America Using NGA Models and Updated Seismological Parameters
Bulletin of the Seismological Society of America, Vol. 101, No. 4, pp. 1859 1870, August 2011, doi: 10.1785/0120100144 Hybrid Empirical Ground-Motion Prediction Equations for Eastern North America Using
More informationGeo-Marine Letters Volume 36, 2016, electronic supplementary material
1 Geo-Marine Letters Volume 36, 016, electronic supplementary material Submarine landslides offshore Vancouver Island along the northern Cascadia margin, British Columbia: why preconditioning is likely
More informationSpatial Correlation of Acceleration Spectral Ordinates from European Data
Spatial Correlation of Acceleration Spectral Ordinates from European Data S. Esposito & I. Iervolino Università degli Studi di Napoli Federico II, Italy SUMMARY Spatial correlation of spectral acceleration
More informationTHE ROLE OF EPSILON FOR THE IDENTIFICATION OF GROUPS OF EARTHQUAKE INPUTS OF GIVEN HAZARD
THE ROLE OF EPSILON FOR THE IDENTIFICATION OF GROUPS OF EARTHQUAKE INPUTS OF GIVEN HAZARD Tomaso TROMBETTI Stefano SILVESTRI * Giada GASPARINI University of Bologna, Italy THE ISSUE 2 THE ISSUE 3 m 3 u
More informationNEXT GENERATION ATTENUATION (NGA) EMPIRICAL GROUND MOTION MODELS: CAN THEY BE USED IN EUROPE?
First European Conference on Earthquake Engineering and Seismology (a joint event of the 13 th ECEE & 30 th General Assembly of the ESC) Geneva, Switzerland, 3-8 September 2006 Paper Number: 458 NEXT GENERATION
More informationGlobal GMPEs. Caribbean Regional Programme Workshop Port of Spain, Trinidad & Tobago, May 2 nd 2011
Caribbean Regional Programme Workshop Port of Spain, Trinidad & Tobago, May 2 nd 2011 Global GMPEs Marco Pagani Executive Committee Hazard Coordinator, GEM Foundation Slides based on C. Di Alessandro presentation
More information7 Ground Motion Models
7 Ground Motion Models 7.1 Introduction Ground motion equations are often called attenution relations but they describe much more than just the attenutation of the ground motion; they describe the probability
More informationAssessment of Point-Source Stochastic Simulations Using Recently Derived Ground-Motion Prediction Equations
Bulletin of the Seismological Society of America, Vol. 99, No. 6, pp. 3172 3191, December 2009, doi: 10.1785/0120080353 Assessment of Point-Source Stochastic Simulations Using Recently Derived Ground-Motion
More informationDeterministic Generation of Broadband Ground Motions! with Simulations of Dynamic Ruptures on Rough Faults! for Physics-Based Seismic Hazard Analysis
Deterministic Generation of Broadband Ground Motions! with Simulations of Dynamic Ruptures on Rough Faults! for Physics-Based Seismic Hazard Analysis Zheqiang Shi and Steven M. Day! Department of Geological
More informationOccurrence of negative epsilon in seismic hazard analysis deaggregation, and its impact on target spectra computation
Occurrence of negative epsilon in seismic hazard analysis deaggregation, and its impact on target spectra computation Lynne S. Burks 1 and Jack W. Baker Department of Civil and Environmental Engineering,
More informationToward a Ground-Motion Logic Tree for Probabilistic Seismic Hazard Assessment in Europe
Toward a Ground-Motion Logic Tree for Probabilistic Seismic Hazard Assessment in Europe Elise Delavaud, Fabrice Cotton, Sinan Akkar, Frank Scherbaum, Laurentiu Danciu, Céline Beauval, Stéphane Drouet,
More informationDeveloping ENA GMPE s Using Broadband Synthe=c Seismograms from Finite- Fault Simula=ons
Developing ENA GMPE s Using Broadband Synthe=c Seismograms from Finite- Fault Simula=ons Art Frankel U.S. Geological Survey SeaFle, WA NGA- East workshop Oct 29, 2014 From Frankel (2009) 1 ENA broadband
More information