<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>10</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/nhess-10-923-2010</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/10/923/2010/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/10/923/2010/nhess-10-923-2010.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/10/923/2010/nhess-10-923-2010.pdf</fulltext_pdf>
	<start_page>923</start_page>
	<end_page>932</end_page>
	<publication_date>2010-04-27</publication_date>
	<article_title content_type="html">Rapid characterisation of large earthquakes by multiple seismic broadband arrays</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Roessler</name>
			<email>d-roessler@web.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Krueger</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Ohrnberger</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>L. Ehlert</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth and Environmental Studies, University of Potsdam, K.-Liebknecht-Str. 24/H27, 14476 Potsdam, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">An automatic procedure is presented to retrieve rupture parameters for large
earthquakes along the Sunda arc subduction zone. The method is based on
standard array analysis and broadband seismograms registered within
30°–100° epicentral distance. No assumptions on source
mechanism are required. By means of semblance the coherency of &lt;i&gt;P&lt;/i&gt; waveforms
is analysed at separate large-aperture arrays. Waveforms are migrated to a
10°&amp;times;10° wide source region to study the spatio-temporal
evolution of earthquakes at each array. The multiplication of the semblance
source maps resulting at each array increases resolution. Start, duration,
extent, direction, and propagation velocity are obtained and published within
25 min after the onset of the event. First preliminary results can be
obtained even within 16 min. Their rapid determination may improve the
mitigation of the earthquake and tsunami hazard. Real-time application will
provide rupture parameters to the GITEWS project (German Indonesian
Tsunami Early Warning System). The method
is applied to the two &lt;i&gt;M&lt;/i&gt;8.0 Sumatra earthquakes on 12 September 2007, to
the &lt;i&gt;M&lt;/i&gt;7.4 Java earthquake on 2 September 2009, and to major subduction
earthquakes that have occurred along Sumatra and Java since 2000. Obtained
rupture parameters are most robust for the largest earthquakes with
magnitudes &lt;i&gt;M&lt;/i&gt;&amp;ge;8. The results indicate that almost the entire seismogenic
part of the subduction zone off the coast of Sumatra has been ruptured. Only
the great Sumatra event in 2004 and the &lt;i&gt;M&lt;/i&gt;7.7 Java event on 17 July 2006
could reach to or close to the surface at the trench. Otherwise, the
rupturing was apparently confined to depths below 25 km. Major seismic gaps
seem to remain off the coast of Padang and the southern tip of Sumatra.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Aki, K. and Richards, P.: Quantitative seismology, University Science Books, Sausalito, 2002. </reference>
		<reference numeration="2" content_type="text"> Douze, E J. and Laster, S J.: Statistics of semblance, Geophysics, 44, 1999–2003, \doi10.1190/1.1440953, short Note, 1979. </reference>
		<reference numeration="3" content_type="text"> Ekström, G. and Nettles, M.: The Global CMT Project, online available at: prefixhttp://www.globalcmt.org, last access: October 2009, 2009. </reference>
		<reference numeration="4" content_type="text"> Gudmundsson, O. and Sambridge, M.: A regionalized upper mantle (RUM) seismic model., J. Geophys. Res., 103, 7121–7136, 1998. </reference>
		<reference numeration="5" content_type="text"> Hanka, W., Heinloo, A., and Jaeckel, K.-H.: Networked Seismographs: GEOFON Real-Time Data Distribution, Orfeus Newsletter, 2, 24, prefixhttp://www.orfeus-eu.org/Organization/Newsletter/vol2no3/geof% on.html, 2000. </reference>
		<reference numeration="6" content_type="text"> Ishii, M., Shearer, P., and Vidale, J.: Extent, duration and speed of the 2004 Sumatra-Andaman earthquake imaged by the Hi-Net array, Nature, 435, 933–936, \doi10.1038/nature03675, 2005. </reference>
		<reference numeration="7" content_type="text"> Ishii, M., Shearer, P M., Houston, H., and Vidale, J E.: Teleseismic $P$ wave imaging of the 26 December 2004 Sumatra-Andaman and 28 March 2005 Sumatra earthquake ruptures using the Hi-net array, J. Geophys. Res., 112, B11307, \doi10.1029/2006JB004700, 2007. </reference>
		<reference numeration="8" content_type="text"> Kennett, B., Engdahl, E., and Buland, R.: Constraints on seismic velocities in the Earth from travel times, Geophys. J. Int., 122, 108–124, 1995. </reference>
		<reference numeration="9" content_type="text"> Krüger, F. and Ohrnberger, M.: Tracking the rupture of the $M_W=9.3$ Sumatra earthquake over 1150 km at teleseismic distance, Nature, 435, 937–939, \doi10.1038/nature0369kao, 2005. </reference>
		<reference numeration="10" content_type="text"> Krüger, F., and M. Ohrnberger: Spatio-temporal source characteristics of the 26 December 2004 Sumatra earthquake as imaged by teleseismic broadband arrays, Geophys. Res. Lett., 32, L24312, doi:10.1029/2005GL023939, 2005. </reference>
		<reference numeration="11" content_type="text"> Krüger, F., Rößler, D., and Ohrnberger, M.: Rupture propagation of the July 17, 2006, Mw=7.7 TsE off-coast Java, in: Eos Trans. AGU, vol 87 of Fall Meet. Suppl., Abstract S21A-0127\/, 2006. </reference>
		<reference numeration="12" content_type="text"> Neiddell, N. and Turhan~Taner, M.: Semblance and other coherency measures for multichannel data, Geophysics, 36, 482–497, 1971. </reference>
		<reference numeration="13" content_type="text"> Ohrnberger, M. and Krüger, F.: Imaging of Large Earthquake Rupture Processes Using Multiple Teleseismic Arrays: Application to the Sumatra-Andaman Island, in: Eos Trans. AGU, vol 86 of Fall Meet. Suppl., Abstract U11A-0819\/, 2005. </reference>
		<reference numeration="14" content_type="text"> Rößler, D., Krüger, F., and Ohrnberger, M.: Rupture Propagation of the 2008/05/12 Ms8.0 Wenchuan Earthquake Using Multiple Teleseismic Arrays, in: Eos Trans. AGU, vol 89 of Fall Meet. Suppl. Abstract S31B-1908\/, 2008. </reference>
		<reference numeration="15" content_type="text"> Rößler, D., Krüger, F., Ohrnberger, M., and Ehlert, L.: Teleseismic rupture tracking of large earthquakes, online available at: prefixhttp://www.uni-potsdam.de, 2009. </reference>
		<reference numeration="16" content_type="text"> Rost, S. and Thomas, C.: Improving Seismic Resolution Through Array Processing Techniques, Surv. Geophys., 30, 271–299, \doi10.1007/s10712-009-9070-6, 2009. </reference>
		<reference numeration="17" content_type="text"> Rudloff, A., Lauterjung, J., Münch, U., and Tinti, S.: Preface &quot;The GITEWS Project (German-Indonesian Tsunami Early Warning System)&quot;, Nat. Hazards Earth Syst. Sci., 9, 1381–1382, 2009. </reference>
		<reference numeration="18" content_type="text"> Subarya, C., Chlieh, M., Prawirodirdjo, L., Avouac, J.-P., Bock, Y., andA. J Meltzner, K S., Natawidjaja, D H., and McCaffrey, R.: Plate-boundary deformation associated with the great Sumatra Andaman earthquake, Nature, 440, 46–51, \doi10.1038/nature04522, 2006. </reference>
		<reference numeration="19" content_type="text"> Weber, B., Becker, J., Hanka, W., Heinloo, A., Hoffmann, M., Kraft, T., Pahlke, D., Reinhardt, J., Saul, J., and Thoms, H.: SeisComP3 – automatic and interactive real time data processing, in: Geophysical Research Abstracts, vol 9 of EGU General Assembly\/, 2007. </reference>
		<reference numeration="20" content_type="text"> Xu, Y., Koper, K D., Sufri, O., Zhu, L., and Hutko, A R.: Rupture imaging of the $M_w 7.9$ 12 May 2008 Wenchuan earthquake from back projection of teleseismic $P$ waves, Geochem. Geophy. Geosy., 10, Q04006, \doi10.1029/2008GC002335, 2009. </reference>
		<reference numeration="21" content_type="text"> Zhang, H., Xu, L., Chen, Y., Li, C.-l., and Stammler, K.: Frequency-domain array technique analysis for the rupture duration time and geometrical characteristics of the 2001 Kunlun Mountain Pass earthquake, Acta Seismologica Sinca, 21, 11–23, \doi10.1007/s11589-008-0011-0, 2008. </reference>
	</references>
</article>

