A Prototype Earthquake Early Warning (EEW) System in Beijing Capital Region of China

Similar documents
Ground motion attenuation relations of small and moderate earthquakes in Sichuan region

Earthquake magnitude estimation using the s c and P d method for earthquake early warning systems

"The Big One" by sea and not by land

INTRODUCTION AND PRELIMINARY ANALYSIS OF STRONG MOTION RECORDINGS FROM THE 12 MAY 2005 Ms8.0 WENCHUAN EARTHQUAKE OF CHINA

Seismic Hazard and Risk Assessments for Beijing Tianjin Tangshan, China, Area

SIMULATED SEISMOGRAMS

Characteristics and introduction of Earthquake in Asia-Pacific region

Effects of Surface Geology on Seismic Motion

Exploring the feasibility of on-site earthquake early warning using close-in records of the 2007 Noto Hanto earthquake

Tomographic imaging of P wave velocity structure beneath the region around Beijing

Study on the Effect of Loess Sites on Seismic Ground Motion and Its Application in Seismic Design

Progress on Development of an Earthquake Early Warning System Using Low-Cost Sensors

To Construct the Theory and Practice System of Integrated Disaster Risk Management

Once you have opened the website with the link provided choose a force: Earthquakes

Regulations on Administration of Earthquake Predictions

Development and Application of Earthquake Early Warning System in NCREE. P.Y. Lin, T.Y. Hsu & H.W. Jiang

Relationships between ground motion parameters and landslides induced by Wenchuan earthquake

TEGAM s Connection to the EarthScope Project

20.1 Earthquakes. Chapter 20 EARTHQUAKES AND VOLCANOES. Earthquakes and plate boundaries 500 UNIT 6 EARTH S STRUCTURE

Earthquake Lab Introduction: Purpose: Method: Equipment needed: Fundamental Concepts and Key Terms:

14 State of the Art and Progress in the Earthquake Early Warning System in Taiwan

How to Use This Presentation

Strong Motion, Damage, and Loss of Wenchuan Earthquake

FEASIBILITY STUDY ON EARTHQUAKE EARLY WARNING SYSTEM FOR THE CITY OF LIMA, PERU, USING A NEWLY DEPLOYED STRONG-MOTION NETWORK

Earthquake information

Epicenter - a point, directly above the true center of disturbance, from which the shock waves of an earthquake apparently radiate.

Brief introduction to recovery and reconstruction

A STUDY ON THE GROUND MOTION CHARACTERISTICS OF TAIPEI BASIN, TAIWAN, BASED ON OBSERVED STRONG MOTIONS AND MEASURED MICROTREMORS

Estimation of Deep Shear-Wave Velocity Profiles in Lima, Peru, Using Seismometers Arrays

Negative repeating doublets in an aftershock sequence

I. Locations of Earthquakes. Announcements. Earthquakes Ch. 5. video Northridge, California earthquake, lecture on Chapter 5 Earthquakes!

Magnitude determination using strong groundmotion attenuation in earthquake early warning

Why 1G Was Recorded at TCU129 Site During the 1999 Chi-Chi, Taiwan, Earthquake

Earthquakes and Earth s Interior

What causes an earthquake? Giant snakes, turtles, catfish, and spiders?

UC Berkeley Berkeley Scientific Journal

Predicting Structural Response with On-Site Earthquake Early Warning System Using Neural Networks

Figure Locations of the CWB free-field strong motion stations, the epicenter, and the surface fault of the 1999 Chi-Chi, Taiwan earthquake.

e-science on Earthquake Disaster Mitigation in Taiwan

Developing a Prototype Earthquake Early Warning System in the Beijing Capital Region

Seismic and Tsunami Observations of Indonesia

Objective: You will learn to interpret a seismogram and, using differences in seismic waves, locate the epicenter of an earthquake.

29th Monitoring Research Review: Ground-Based Nuclear Explosion Monitoring Technologies

EARTHQUAKE PREDICTION RESEARCH IN CHINA: STATUS AND PROSPECTS

GENERAL. CHAPTER 1 BACKGROUND AND PURPOSE OF THE GUIDELINES Background of the Guidelines Purpose of the Guidelines...

Activities and Outlook related to Disaster Reduction in CMA

New Findings Form Basis for Earthquake

A. Locate the Epicenter

Development of A Rapid Typhoon Loss Estimation System in China

California s New Earthquake Early Warning System And Why We Are Different

Seismic Response Analysis of selected sites in Wenxian urban area, China

CASUALTY IN EARTHQUAKE AND TSUNAMI DISASTERS: INTERNET-BASED MONITORING AND EARLY ESTIMATION OF THE FINAL DEATH TOLL

Determining the Earthquake Epicenter: Japan

Earthquakes in Ohio? Teacher Directions and Lesson

M-6.2 EARTHQUAKE NORCIA, ITALY AUGUST 24, 01:36:33 UTC

Seismic Risk Assessments for Border Area of Shanxi, Hebei and Inner Mongolia, China

Name: Date: Bell: The Sumatra Earthquake and Tsunami December 26, 2004

State of art of seismic design and seismic hazard analysis for oil and gas pipeline system

JCR (2 ), JGR- (1 ) (4 ) 11, EPSL GRL BSSA

THE 2011 TOHOKU EARTHQUAKE IN JAPAN. VSU Lyuben Karavelov, Sofia, Bulgaria. Key words: Tohoku earthquake, strong ground motion, damage

中村洋光 Hiromitsu Nakamura 防災科学技術研究所 National Research Institute for Earth Science and Disaster Prevention, Japan (NIED) Outline

Prentice Hall EARTH SCIENCE

Study on Shandong Expressway Network Planning Based on Highway Transportation System

Earthquake early warning: Adding societal value to regional networks and station clusters

2/8/2016 Magnitude-6.3 earthquake near Tainan, Taiwan, highlights the danger of blind thrust faults around the world

What is an Earthquake?

Earthquakes Modified

Earthquake Hazard Analysis Methods: A Review

REPORT ON THE TOHOKU AREA PASIFIC OFFSHORE EARTHQUAKE

The 2016, October 26, Central Italy Earthquake Origin Time 17:10:36 UTC, M L(ISNet) =5.3; M W(ISNet) =5.6

DATA BASE DEVELOPMENT OF ETA (ESTIMATED TIME OF ARRIVAL) FOR TSUNAMI DISASTER MITIGATION AT SOUTHWESTERN CITIES OF ACEH, INDONESIA

Magnitude 7.1 NEAR THE EAST COAST OF HONSHU, JAPAN

Coping with natural risk in the XXI century: new challenges for scientists and decision makers

Earthquake Early Warning Technology Progress in Taiwan

SHAKE, RATTLE, AND ROLL INVESTIGATING EARTHQUAKES

Determination of earthquake early warning parameters, τ c and P d, for southern California

This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and

Possible Abnormal Phenomenon of the Atmospheric Water Vapor before Hengchun Earthquake

Seismic Quiescence before the 1999 Chi-Chi, Taiwan, M w 7.6 Earthquake

GIS SUPPORTED ANALYSIS ON CITY GATHERING IN CHINA. Ren Fuhu

LAB. Balboa Heights, Panama. Boulder, Colorado. Mexico City, Mexico. Data Table. Difference Between P-wave and S-wave. S-wave Arrival Time

Establishment and Operation of a Regional Tsunami Warning Centre

Practical Use of the Earthquake Early Warning (EEW) System for Shinkansen

EARTH OBSERVATION SERVICES IN REPUBLIC OF MOLDOVA

EARTHQUAKE EARLY WARNING SYSTEM AT A LOCAL GOVERNMENT AND A PRIVATE COMPANY IN JAPAN

FOURTH GRADE HAZARDS 1 WEEK LESSON PLANS AND ACTIVITIES

PI Forecast for the Sichuan-Yunnan Region: Retrospective Test after the May 12, 2008, Wenchuan Earthquake

THE STUDY ON 4S TECHNOLOGY IN THE COMMAND OF EARTHQUAKE DISASTER EMERGENCY 1

International Cooperation on Earthquake Disaster Management to Protect Lives

Disaster Risk Reduction in Survey for Seismic Protection of MES

2.3 Notes: Earthquake Damage Can Be Reduced

Sampling Scheme for 2003 General Social Survey of China

Dangerous tsunami threat off U.S. West Coast

What Are Recorded In A Strong-Motion Record?

Name Date Class. radiate in all directions, carrying some of the. of plate boundaries have different usual patterns of.

How Do Scientists Find the Epicenter of an Earthquake?

Integrated Science I: Locating earthquake epicenters. Name Per Date

EXECUTIVE SUMMARY. The title of this dissertation is Quantitative Study on Natural Disasters Risk

Disclaimer. This report was compiled by an ADRC visiting researcher (VR) from ADRC member countries.

Japan Seismic Hazard Information Station

Transcription:

The 2th International Workshop On Earthquake Early Warning, April 21-22, 2009, Kyoto, Japan A Prototype Earthquake Early Warning (EEW) System in Beijing Capital Region of China Hanshu Peng 1, Zhongliang Wu 1, Yang Xu 2, Changsheng Jiang 1 1. Institute of Geophysics, China Earthquake Administration 2. Labs of China United Network Communications Corporation Limited

In history, earthquake has brought our world with uncountable criminals! Is it possible to catch it? Unpredictable Instantaneous Extremely Strong Social Impact Secondary Disaster Direct Damage

The Original Concept of EEW 3 November 1868 Editor, San Francisco Daily Evening Bulletin:... we are now obliged to look for some... means of prognosticating [earthquakes] and I wish to suggest the following mode by which we may make electricity the means, perhaps, of saving thousands of lives in case of the occurrence of more severe shocks than we have yet experienced... If this center happens to be far enough from [San Francisco], we may be easily notified of the coming wave in time for all to escape from dangerous buildings before it reaches us...... A very simple mechanical contrivance can be arranged at various points from 10 to 100 miles from San Francisco, by which a wave of the earth high enough to do damage will start an electric current over the wires now radiating form this city and almost instantaneously ring an alarm bell... J. D. Cooper, M.D. San Francisco, California

Recent 10 years EEW has been developed rapidly both on theory and technology. In Japan, California, Taiwan, Mexico, Turkey and so on, EEW systems have shown significant potential for the earthquake disaster reduction.

Earthquakes in China (since 1900) Serious earthquake situation in continental Herbin China calls for EEW system! Wulumuqi Shenyang Beijing Lanzhou Xian Lasa Chendu Wuhan Shanghai 5.0-5.9 6.0-6.9 7.0-7.9 Kunming Guangzhou Taipei >=8.0 It is still blank for EEW system in continental China

May 12, 2008, 14:28 local time M S 8.0 Wenchuan earthquake caused tremendous loss of property and life, if there is a welloperating EEW system Casualty ~70,000 Injury ~370,000 Missing ~18,000 Affected ~45.7M people Economic Loss ~ 8kM RMBY The occurrence of 2008 Wenchuan Earthquake highlighted the importance of constructing earthquake early warning (EEW) system in continental China.

At present, it is impossible to construct EEW for all regions of China. A famous saying let some people be rich first leads to today s prosperity of continental China. Mr. Xiaoping Deng, an outstanding leader of China We should let some regions construct EEW system first.

As the beginning As attempts of EEW system construction, several projects related to EEW have been conducted in continental China. In Fujian Province: Fast report of earthquake parameters within 1 minute after the earthquake In Beijing Capital Region: A prototype EEW system is under construction, which will be introduced in this workshop

Prototype EEW in Beijing Capital Region Demand and Foundation Progress in theoretical problem Prototype system construction

Peak Ground Acceleration Zonation Map of Continental China Location of Beijing Capital Region (with higher peak ground acceleration) (38.5-41.5 N, 113.5-120 E)

Demands of EEW System in Beijing Capital Region Politic, Historical economic, Distribution and culture in Beijing center of Capital ChinaRegion Mass population Seismic potential 1679 Sanhe- Pinggu M8.0 Earthquake 1976 Tangshan M7.8 Earthquake So, it is necessary and urgent to develop EEW system in this region.

Beijing Capital Seismic Network (BCSN) Platform Foundation Total 135 stations with average inter-station distance about 50 km, local reach to 20km. Broadband: 74 Very Broadband:3 Short-period:58

Prototype EEW in Beijing Capital Region Demand and Foundation Progress on theoretical problems Prototype system construction

Theoretical Problems on EEW in Beijing Capital Region As preparatory work of EEW construction in Beijing Capital Region, we have done some theoretical research on EEW. Saturation of magnitude estimation associated with short-period recordings Empirical relations for the estimation of magnitude using the first 3-second P waves Capability evaluation of EEW

Theoretical Problem in EEWS Construction in Beijing Capital Region: Magnitude saturation M Magnitude threshold Broadband Short-period saturation Broadband instrument is widely used to EEW due to the magnitude saturation caused by short-period recording. But there are so many short-period seismographs deployed in BCSN. M

Theoretical Problem in EEWS Construction in Beijing Capital Region: Magnitude saturation To investigate the possibility of using short-period recording to EEW, we conducted a testing with 1999 Chi-chi earthquake and its 32 aftershocks. TSMIP 32 events of Chi-Chi earthquak e

Theoretical Problem in EEWS Construction in Beijing Capital Region: Magnitude saturation Convolving the strong motion acceleration recordings in Taiwan with the instrument response of short-period seismographs in Beijing Capital Region, we get the simulated short-period recording of Beijing Capital Region to the same event. The first few seconds after the P-arrival, especially for the first 3 seconds, the strong motion recording and the simulated short-period one are similar to each other.

Theoretical Problem in EEWS Construction in Beijing Capital Region: Magnitude saturation Comparison between Broadband Recordings and Shortperiod Recordings Using P d Measurement X-coordinate: Original Magnitude Y-coordinate: Estimated Magnitude Saturation appears with short-period recording for large earthquake upper 6, no obvious difference for middle earthquake.

Theoretical Problem in EEWS Construction in Beijing Capital Region: Magnitude saturation Comparison between Broadband Recordings and Short-period Recordings Using tau_c Measurement Magnitude saturation can be found more obviously in the result of tau_c measurement for large earthquake.

Theoretical Problem in EEWS Construction in Beijing Capital Region: Magnitude saturation Comparison between Using Pd Measurement and Using tau_c Measurement for Short-Period Recording Pd measurement is more preferred than tau_c measurement due to relatively slight magnitude saturation for large earthquake

Theoretical Problem in EEWS Construction in Beijing Capital Region: Frequency compensation A compensation filter was designed to make up for the magnitude estimation loss with short-period recordings.

Magnitude estimation after frequency compensation After compensation, the estimated magnitude was improved obviously for larger size event, especially to tau_c measurement

Theoretical Problem in EEWS Construction in Beijing Capital Region:Magnitude Estimation Empirical magnitude relation by P d measurement M 0.72 log10( Pd) 1.60 log10( R) 3.34

Theoretical Problem in EEWS Construction in Beijing Capital Region:Magnitude Estimation Empirical magnitude relation by tau_c measurement M 1.71 log10( c ) 4.26

Some conclusions Using the first three seconds of the P wave seismograms, short-period recordings can be applied to estimate the size of an earthquake to some extent. By the method of frequency compensation, the problem of magnitude saturation can be solved effectively. When applying short-period seismograph network in the EEW operation, P d measurement is more preferred than tau_c measurement.

Zonation of EEW capability in Beijing Capital Region Compared with the seismic network in Japan, California, and Taiwan, Beijing Capital Seismic Network is not an ideal one for its relatively low density and non-uniform distribution. It is necessary to evaluate it by Estimations of: Warning reporting time Minimum early-warning time Area with high risk of destruction

Zonation of EEW capability in Beijing Capital Region 0.1 0.1

Warning reporting time estimation Supposing earthquake occurred at every grid point we considered with focal depth h=10km, and P wave velocity Vp=6km/s Beijing Area Tianjing Area Tanshan Area The reporting time are all less than 10 seconds in Beijing area and Tianjin area. Tanshan Area is between 10 to 15 seconds.

Minimum early-warning time estimation Supposing earthquake occurred at its historical epicenter with focal depth h=10km, P wave velocity Vp=6km/s and S wave velocity Vs=3.5km/s Beijing Area Tianjing Area Tangshan Area Beijing, Tianjing and Tangshan all have the possibility to have larger blind zone of EEW when earthquake occurs, for their minimum early-warning time is less than zero.

Area with high risk of destruction estimation Pay attention to these areas with PGA>0.2 and the early-warning time is less than zero PGA Map Huailai-Yanqing Basin, Beijing area and Tangshan area ar all with high risk of destruction.

Our present seismic network need to be upgraded ASAP. It s luck that it has been under the new five-year plan of CEA to provide a more ideal platform for EEW.

Prototype EEW in Beijing Capital Region Demand and Foundation Progress in theoretical problems Prototype System construction

In 2007, with the help of Prof. Yih-Min Wu, a testing EEW system was installed to process the data stream at 16 stations.simulated experiments have been conducted.

Prototype EEWS Architecture

Data Processing Flow in the Central Processing Unit Station 1 triggered Calculating c and Pd Station 2 triggered Calculating c and Pd Station 3 triggered Calculating c and Pd Single station magnitude estimation Single Station report logs Station n triggered Calculating c and Pd Real-time seismic waves Multi-Station Processing Events decision Multi-station magnitude and events locating estimation Multi-Station report logs

Prototype EEWS Demo Station CHL triggered estimate c and Pd Station DOH triggered estimate c and Pd Station BDH triggered estimate c and Pd Station ZUH triggered estimate c and Pd

Refining of our prototype is going on Our goal: Constructing a Hybrid EEW system in Beijing Capital Region. 1 Combination of seismographs and strong motion instruments 2 Combination of front-detection EEW and onsite EEW 3 Combination of EEWS and QEDS

Finally, let s recall the tremendous loss of property and life caused by Wenchuan earthquake again Casualty ~70,000 Injury ~370,000 Missing ~18,000 Affected ~45.7M people Loss ~8kM RMBY We hope and believe that all these losses must be compensated by the advancement of earthquake science and technology and the enhancement of the capability of the reduction of seismic disasters not only in China but also all over the world

End of the talk But no ending in EEW system construction EEW in continental China is growing. We are enjoying with international exchange of experiences and international collaborations during the construction of continental China s EEW system.