Seismological Research Letters; March 2008; v. 79; no. 2;
p. 178-185; DOI: 10.1785/gssrl.79.2.178
© 2008 Seismological Society of America
Overview of Open Seismic Data from the North Korean Event of 9 October 2006
Keith D. Koper and
Robert B. Herrmann
Department of Earth and Atmospheric Sciences, Saint Louis
University
Harley M. Benz
U.S. Geological Survey, Denver
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INTRODUCTION
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On 9 October 2006 North Korea announced that it had conducted a nuclear
weapons test, its first, at the Chik-tong test site in north Hamgyeong
Province. It had been more than eight years since the world's last known
nuclear test, carried out by Pakistan on 30 May 1998
(Wallace 1998). The North
Korean event was small (4.2 mb) and occurred in a part of
the world with a relatively low density of accessible (open) broadband
seismometers. Therefore, it provides a nice test of the nuclear explosion
monitoring capability of the open global seismic network, which is deployed
and maintained primarily for the study of earthquakes.
In this study we forgo a comprehensive technical analysis and instead
emphasize the extent to which openly available seismic data and related
products can be used in a forensic sense to study this politically important
event. Much of the material presented here was developed for a discovery-based
course entitled "EAS130 Seismology of Nuclear Weapons," which is
taught to freshmen and sophomores at Saint Louis University.
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EVENT DETECTION AND LOCATION
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The U.S. Geological Survey (USGS) operates the National Earthquake
Information Center (NEIC), a 24/7 seismic monitoring facility with global
earthquake monitoring capabilities and responsibilities (see
http://earthquake.usgs.gov/eqcenter/).
Within or near the Korean peninsula, NEIC's sources of realtime data are
Global Seismic Network (GSN) stations, cooperative stations in China, and
selected stations of the International Monitoring System (IMS). Based on
interstation distances, noise characteristics of individual stations, regional
attenuation properties, and its association and location algorithms, NEIC
estimates that its minimum automatic detection and location threshold for the
Korean peninsula is approximately M 4.5–4.8 (B. Presgrave, personal
communication 2006).
In the week before the North Korean event, a significant number of media
outlets were reporting the possibility of a nuclear test. Consequently, NEIC
staff reviewed its policy and . . . [Full Text of this Article]
Department of Earth and Atmospheric Sciences
Saint Louis
University
3642 Lindell Blvd.
St. Louis, Missouri 63108
USA
kkoper@gmail.com
(K.
D. K.)
Copyright © 2008 by Seismological Society of America