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| The first 20% of the full text of this article appears below. |
| INTRODUCTION |
|---|
Atmospheric shock waves generated by sonic booms, meteoroid falls, and
explosions have been observed in the Center for Earthquake Research and
Information (CERI) Cooperative Seismic Network
(Johnston 1987;
Langston 2004). On 28 January
2004 at 01:58 UTC, 11 short-period and nine broadband CERI network stations
(figure 1) recorded high
signal-to-noise ratio signals generated by an unknown source
(figure 2). A preliminary
analysis of the waveforms and slow velocity across the network suggested that
these signals were not generated by an earthquake but by an acoustic source.
CERI also received several calls from the public in southern Missouri
reporting large booming noises around the time when the event was recorded by
the CERI network (G. Patterson, personal communication, 2005). One of these
reports was from a medical worker in a two-story building in Poplar Bluff,
Missouri. She reported that everyone on the second floor felt a hard jarring
shake and heard a loud explosion, but few felt it on the first floor. The
seismic signals have durations of 30 to 70 s with distinct later arrivals. For
example,
Center for Earthquake Research and Information
University of
Memphis
Memphis, Tennessee
38152
mulas62@yahoo.com
(T.-L.L.)
clangstn@memphis.edu
(C.A.L.)
This article has been cited by other articles:
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J. Pujol and P. Rydelek A Reanalysis of Anomalous Acoustic Signals Recorded by the CERI Seismic Network on 28 January 2004 Seismological Research Letters, May 1, 2007; 78(3): 389 - 393. [Full Text] [PDF] |
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