Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; April 2008; v. 98; no. 2; p. 607-619; DOI: 10.1785/0120060218
© 2008 Seismological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Yamada, M.
Right arrow Articles by Heaton, T.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Real-Time Estimation of Fault Rupture Extent Using Envelopes of Acceleration

Masumi Yamada

Kyoto University, Gokasyo, Uji, 611-0011, Japan masumi{at}eqh.dpri.kyoto-u.ac.jp

Thomas Heaton

California Institute of Technology, MC104-44, 1200 E. California Blvd., Pasadena, California 91125 heaton_t{at}caltech.edu

We present a new strategy to estimate the geometry of a rupture on a finite fault in real time for earthquake early warning. We extend the work of Cua and Heaton who developed the virtual seismologist (VS) method (Cua, 2005), which is a Bayesian approach to seismic early warning using envelope attenuation relationships. This article extends the VS method to large earthquakes where fault finiteness is important. We propose a new model to simulate high-frequency motions from earthquakes with large rupture dimension: the envelope of high-frequency ground motion from a large earthquake can be expressed as a root-mean-squared combination of envelope functions from smaller earthquakes. We use simulated envelopes of ground acceleration to estimate the direction and length of a rupture in real time. Using the 1999 Chi-Chi earthquake dataset, we have run simulations with different parameters to discover which parameters best describe the rupture geometry as a function of time. We parameterize the fault geometry with an epicenter, a fault strike, and two along-strike rupture lengths. The simulation results show that the azimuthal angle of the fault line converges to the minimum uniquely, and the estimation agrees with the actual Chi-Chi earthquake fault geometry quite well. The rupture direction can be estimated at 10 s after the event onset, and the final solution is achieved after 20 s. While this methodology seems quite promising for warning systems, it only works well when there is an adequate distribution of near-source stations.




This article has been cited by other articles:


Home page
Seismological  Research LettersHome page
R. M. Allen, P. Gasparini, O. Kamigaichi, and M. Bose
The Status of Earthquake Early Warning around the World: An Introductory Overview
Seismological Research Letters, September 1, 2009; 80(5): 682 - 693.
[Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by the Seismological Society of America.