Dr. Praveen K. Malhotra, P.E.

Slides:



Advertisements
Similar presentations
Seismic analysis and design of
Advertisements

2nd year SAFER Project meeting. Armada Hotel, Istanbul, Turkey June, Information-dependent lead time maps for earthquake early warning in the.
SÄTEILYTURVAKESKUS STRÅLSÄKERHETSCENTRALEN RADIATION AND NUCLEAR SAFETY AUTHORITY Seismic experience in Finland VN/RA/01 Task 1&2 Workshop Hanoi, October.
EPRI/SOG Mmax –Six earth-science teams, diverse methods largest observed eq (+ increment) catalog statistics – extreme occurrences seismogenic feature:
Ground Motions Geotechnical Earthquake Engineering: Steve Kramer
SEISMIC HAZARD Presentation is based on: Allen, R., Earthquake hazard mitigation: New direction and opportunities, in "Treatise on Geophysics”, Bilham,
Nirmal Jayaram Nilesh Shome Helmut Krawinkler 2010 SCEC Annual Meeting A statistical analysis of the responses of tall buildings to recorded and simulated.
International Insurance-Reinsurance Forum 2012 Managing catastrophic risks From Seismic Hazard Analysis to Seismic Risk mitigation C.O.Cioflan Ph.D., Senior.
Keck Telescope Seismic Upgrade Design Support - Progress Report Frank Kan Andrew Sarawit 4 May 2011 (Revised 5 May 2011)
Acceleration – Magnitude The Analysis of Accelerograms for the Earthquake Resistant Design of Structures.
Deterministic Seismic Hazard Analysis Earliest approach taken to seismic hazard analysis Originated in nuclear power industry applications Still used for.
1 High Performance Computing at SCEC Scott Callaghan Southern California Earthquake Center University of Southern California.
Rupture, Seismic Waves, and Shaking. Earthquake Origins and Seismic Waves –Focus point where earthquake rupture occurs Shallow focus - 70 km or less (80%
Earthquake Hazard Assessment in the Pacific Northwest: Site Response Thomas L. Pratt U. S. Geological Survey School of Oceanography University of Washington.
Characterization of Ground Motion Hazard PEER Summative Meeting - June 13, 2007 Yousef Bozorgnia PEER Associate Director.
Time-dependent seismic hazard maps for the New Madrid seismic zone and Charleston, South Carolina areas James Hebden Seth Stein Department of Earth and.
Studying Earthquakes. Seismology: the study of earthquakes and seismic waves.
DISASTER PREPAREDNESS A KEY ELEMENT OF BECOMING DISASTER RESILIENT Walter Hays, Global Alliance for Disaster Reduction, University of North Carolina,
LESSONS FROM PAST NOTABLE EARTHQUAKES. Part III Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA.
Outline: Lecture 4 Risk Assessment I.The concepts of risk and hazard II.Shaking hazard of Afghanistan III.Seismic zone maps IV.Construction practice What.
New Madrid Earthquake By: Julie Dillon and Caroline Miller.
Paleoseismic and Geologic Data for Earthquake Simulations Lisa B. Grant and Miryha M. Gould.
December 3-4, 2007Earthquake Readiness Workshop Seismic Design Considerations Mike Sheehan.
Chapter 5 EARTHQUAKES and ENVIRONMENT. Earthquakes Violent ground-shaking phenomenon by the sudden release of strain energy stored in rocks One of the.
S OUTHERN C ALIFORNIA E ARTHQUAKE C ENTER Themes by Tom Henyey.
Structural Engineering Issues for a Large Cascadia Event.
Cascadia Subduction Zone Earthquakes and Critical Infrastructure Workshop Edward Perez, FERC Background - Part 12D Report. - Every 5 years. - Top-to-bottom.
Intraplate Deformation and Seismicity: Implication for Seismic Hazard and Risk Estimates in the Central United States Zhenming Wang Kentucky Geological.
Seismic Hazard Assessment for the Kingdom of Saudi Arabia
Earthquake Hazard Session 1 Mr. James Daniell Risk Analysis
Real World Applications of USGS EQ Science: Stacy Bartoletti Degenkolb Engineers Structural Engineers Association of Washington Cascadia Region Earthquake.
1 Risk comments including some Re-insurance issues (Socio-Economic Security)  Jorge A. Prieto, PhD. PEng.  Natural Resources Canada, Geological Survey.
Michael Hodges, Chris Kohlenberger, Nolan Mattox, and Christian Vanderwall Seismic Hazard Map Plugin Improvement of ShakeMap Plugin Custom Color Maps Team.
Engineering Geology and Seismology
Earthquake Science (Seismology). Seismometers and seismic networks Seismometers and seismic networks Earthquake aftershocks Earthquake aftershocks Earthquake.
1. 2 CE-312 Engineering Geology and Seismology Instructor: Dr Amjad Naseer Lecture#15 Department of Civil Engineering N-W.F.P University of Engineering.
Estimation of Future Earthquake Annualized Losses in California B. Rowshandel, M. Reichle, C. Wills, T. Cao, M. Petersen, and J. Davis California Geological.
Living in Earthquake Country Concept Maps. Overview Evidence from past earthquakes can help us predict the amount of damage to expect from future earthquakes.
Earthquake hazard isn’t a physical thing we measure. It's something mapmakers define and then use computer programs to predict. To decide how much to believe.
SEISMIC HAZARD. Seismic risk versus seismic hazard Seismic Hazard is the probability of occurrence of a specified level of ground shaking in a specified.
LESSONS FROM PAST NOTABLE EARTHQUAKES. Part IV Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA.
Probabilistic Ground Motions for Scoggins Dam, Oregon Chris Wood Seismotectonics & Geophysics Group Technical Service Center July 2012.
Loss-Estimation Modeling of Earthquake Scenarios for Each County in Nevada Using HAZUS-MH Nevada Bureau of Mines and Geology Open-File Report 06-1 University.
2004 CAS RATEMAKING SEMINAR INCORPORATING CATASTROPHE MODELS IN PROPERTY RATEMAKING (PL - 4) PRICING EARTHQUAKE INSURANCE DAVE BORDER, FCAS, MAAA.
Epistemic Uncertainty on the Median Ground Motion of Next-Generation Attenuation (NGA) Models Brian Chiou and Robert Youngs The Next Generation of Research.
9. As hazardous as California? USGS/FEMA: Buildings should be built to same standards How can we evaluate this argument? Frankel et al., 1996.
1J. Baker Jack Baker Civil & Environmental Engineering Stanford University Use of elastic & inelastic response spectra properties to validate simulated.
Probabilistic seismic hazard assessment for the pseudo-negative stiffness control of a steel base-isolated building: A comparative study with bilinear.
4th International Conference on Earthquake Engineering Taipei, Taiwan October 12-13, 2006 Site-specific Prediction of Seismic Ground Motion with Bayesian.
Tri-State Seismic Hazard Mapping -Kentucky Plan
Understanding Earth Sixth Edition Chapter 13: EARTHQUAKES © 2011 by W. H. Freeman and Company Grotzinger Jordan.
Antonella Peresan F. Vaccari, A. Magrin, G.F. Panza, S. Cozzini B.K. Rastogi, I. Parvez Antonella Peresan F. Vaccari, A. Magrin, G.F. Panza, S. Cozzini.
Metrics, Bayes, and BOGSAT: Recognizing and Assessing Uncertainties in Earthquake Hazard Maps Seth Stein 1, Edward M. Brooks 1, Bruce D. Spencer 2 1 Department.
Earthquake Site Characterization in Metropolitan Vancouver Frederick Jackson Supervisor – Dr. Sheri Molnar.
Printout 4 slides per page, give for questions by
Earthquakes.
British Seismology Meeting 5th – 7th April 2017, Reading, UK
How the ground shakes? Dr. Syed Mohamed Ibrahim M.Tech., Ph.D., by
NGA-East Tentative Plan
CE 5603 Seismic Hazard Assessment
Warm Up A stretched spring attached to two fixed points is compressed on one end and released. The resulting wave travels back and forth between the two.
Philip J. Maechling (SCEC) September 13, 2015
Understanding Earth Chapter 13: EARTHQUAKES Grotzinger • Jordan
Earthquakes Photo credit: USGS.
VII. Earthquake Mitigation
Engineering Geology and Seismology
Engineering Geology and Seismology
Seismic Eruption - forecasting future earthquakes
Deterministic Seismic Hazard Analysis
Earthquakes.
Presentation transcript:

Dr. Praveen K. Malhotra, P.E. Ground Motion Histories for Seismic Design of Kingdom Tower in Saudi Arabia Contact Information: Praveen.Malhotra@StrongMotions.com www.StrongMotions.com 781-363-3003 Dr. Praveen K. Malhotra, P.E. SEAOA Convention, Tucson, Arizona June 18-20, 2015

Outline Engineering Perspective of Probabilistic Seismic Hazard Analysis (PSHA) Ground Motion Histories for Seismic Design of Kingdom Tower in Saudi Arabia

Overview Structural Geotechnical Seismological Geological

Where Will Future Earthquakes Occur?

Where Will Future Earthquakes Occur?

How Big Will They be and When Will They Occur? Mw 6 @ 794 years MRI Mw 6.1 @ 977 years MRI Mw 6.2 @ 1202 years MRI Mw 6.3 @ 1479 years MRI Mw 6.4 @ 1820 years MRI Mw 6.5 @ 2240 years MRI

How Strong Will the Ground Shake During a Magnitude M 7 How Strong Will the Ground Shake During a Magnitude M 7.5 Earthquake at 20 km?

How Strong Will the Ground Shake During a Magnitude M 7 How Strong Will the Ground Shake During a Magnitude M 7.5 Earthquake at 20 km?

Probabilistic Seismic Hazard Analysis Geological and seismological models are so uncertain that only probabilistic predictions can be made regarding ground shaking

Peak Ground Acceleration Hazard Curve for a Site in Los Angeles

Maximum Acceleration in 50 Years µ = 0.208 g = 0.211 g COV = /µ = 1.01

Geographical Variation of Uncertainty City µ (g)  (g) COV = /µ Los Angeles 0.208 0.21 1.01 San Francisco 0.189 0.9 Memphis 0.083 0.177 2.15 Boston 0.023 0.07 3.11

Why Does Uncertainty Matter?

Expected and Design Acceleration µPGA = 0.208 g DesignPGA = 0.536 g

Expected and Design Accelerations for Different Cities City Expected (g) Design (g) Design/Expected Los Angeles, CA 0.208 0.536 2.6 San Francisco, CA 0.21 0.514 2.4 Memphis, TN 0.0669 0.345 5.2 Boston, MA 0.0226 0.0946 4.2 Uncertainty increases the cost of mitigation

Uncertainty increases the cost of insurance Return Period of Collapse for Same Ratio Between Expected and Design Accelerations City MRP of Collapse Los Angeles, CA 4250 years San Francisco, CA 5000 years Memphis, TN 1500 years Boston, MA 2200 years Uncertainty increases the cost of insurance

Design Versus Expected Annual Acceleration City Expected (g) Design (g) Design/Expected Los Angeles, CA 0.0113 0.536 47 San Francisco, CA 0.0108 0.514 48 Memphis, TN 0.00212 0.345 163 Boston, MA 0.00053 0.0946 178 Uncertainty makes mitigation less attractive than insurance

Effects of Uncertainty Increased cost of mitigation Increased cost of insurance Voluntary mitigation becomes less attractive compared to insurance, but insurance cannot reverse: Loss of life Loss of business Damage to environment Insurance without mitigation is costly

Historic Variation of Uncertainty 50-year Maximum PGA COV = /µ 1996 0.25 0.188 0.75 2002 0.258 0.2 0.78 2008 0.234 0.221 0.95 2014 0.208 0.21 1.01 Geoscientists are less certain now than in 1996

Reasons for Increased Uncertainty As computers became faster and more powerful, it became possible for the USGS to consider more sources of uncertainty in the PSHA The number of opinions regarding the geological and seismological models increased over the years due to a greater number of researchers investigating the seismic hazard Seismic hazard analysis is in its early stages and geoscientists are still discovering more and more that they do not know

Significance of Change Between the Results of Successive PSHA Effect size, d = (µ1 - µ2)/ d > 0.8 is large change d ~ 0.5 is moderate change d < 0.2 is small change Cohen, J. (1988). Statistical Power Analysis for the Behavioral Sciences (second ed.), New Jersey, Lawrence Erlbaum Associates.

Significance of Change Between the Results of Successive PSHA Interval Effect-Size of Change 1996-2002 0.04 2002-2008 0.11 2008-2014 0.12 Changes in ground motion predictions were statistically insignificant

Suggestions to Avoid Misuse of PSHA PSHA should not be considered as an excuse for using models with high uncertainty. Models with high uncertainty increase the costs of mitigation and insurance. There is a common misconception that uncertainty does not matter as long as it can be modeled in the PSHA

Suggestions to Avoid Misuse of PSHA The focus in seismic hazard analysis should shift from considering uncertainty to reducing uncertainty. In the seismic hazard community, there are more discussions on considering uncertainty, and practically no discussions on reducing uncertainty. The real progress in the science of ground motion prediction can only be made by reducing uncertainty

Suggestions to Avoid Misuse of PSHA Uncertainty in geological and seismological models should be reduced by gradually replacing empirical models with physics-based models and by limiting the number of opinions considered in the PSHA. Empirical models, by their very nature, are uncertain and there are several opinions regarding empirical models. For example, at present time, there are about 300 ground motion prediction models in the published literature.

Suggestions to Avoid Misuse of PSHA The design ground motions should not be revised unless a statistically significant change occurs in the predicted ground motions. The uncertainty in ground motion prediction is so high that a slight changes in ground motion estimates do not justify a change in the design ground motions

Suggestions to Avoid Misuse of PSHA Site-specific PSHA should not be used for the sole purpose of reducing design ground motions. Since there are many opinions regarding geological and seismological models, a combination of opinions can be easily found which provides a lower estimate of the design ground motion. This practice should be stopped, because it provides a biased assessment of the risk

Suggestions to Avoid Misuse of PSHA Same predictions of ground motions should be used for seismic design and insurance of all types of structures. There is no convincing argument for separate PSHA for buildings, bridges, dams and nuclear power plants. Design ground motions should be different for different types of structures, based on the consequence of damage; but the underlying assessment of the hazard should be the same

Suggestions to Avoid Misuse of PSHA Seismic hazard models should not be made more complex unless they reduce uncertainty. It does not make sense for ground motion prediction models to become more complex and less certain at the same time. Complexity without certainty is self-serving

Ground Motion Histories for Seismic Design of Kingdom Tower

Seismic Map of Region According to USGS Kingdom Tower

Propagation of High- and Low-Frequencies

2475-year MRP Response Spectrum from PSHA by Langan International

Earthquake Scenarios Controlling the Seismic Hazard Natural Period, T (s) Magnitude, Mw Distance (km) 0.3 5.9 70  4 7.1 1000

Long-Period Transition for Different Magnitude Earthquakes (NEHRP 2003) Magnitude Mw TL (s) 6.0 – 6.5 4 6.5 – 7.0 6 7.0 – 7.5 8 7.5 – 8.0 12 8.0 – 8.5 16 8.5 – 9.0+ 20

2475-year MRP Response Spectrum

Target Response Spectrum for Closer-Smaller Earthquakes

Target Response Spectrum for Distant-Larger Earthquakes

Vertical Response Spectra for Closer and Distant Earthquakes

‘Seed’ Ground Motion for Closer Earthquake Scenario

Response Spectra of ‘Seed’ Ground Motion for Closer Earthquake Scenario

Response Spectra of Modified Horizontal Components

Response Spectra of Modified Horizontal and Vertical Components

Comments High-rise buildings respond to ground displacements rather than ground accelerations Site-specific free-surface ground motions do not depend on the structure being analyzed; they depend only on the geology and seismology of the region All three components of a ground motion need to be simultaneously modified to make it site-specific