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Ground Motion Waveforms of 9:55AM, May 25th, 2009 Launched:
May 25, 20009
Updated:
May 28, 2009


According to USGS, an event occurred at 9:54:43AM, May 25th 2009 (Japan time), in the vicinity of North Korea. The observed ground motions from this event show features different from a natural earthquake. We will update information on this event occasionally (Outreach Office).


[Observed Waveform]

The ground motions recorded on May 25th, around 9:55AM (Japan time), were observed with a high-sensitivity seismograph network of the National Research Institute for Earth Science and Disaster Prevention (NIED) .

According to USGS, the source of this event is located at lat=41.331 N,lon=129.011 E,depth=0km. The vertical axis indicates the distance from the source, and the horizontal axis shows the lapse time from 9:56:00AM.

(Click to enlarge)

[Comparison with natural earthquakes - No.1]
The following compares the observed waveforms from this event (Left) with those from the natural earthquake, which occurred in the vicinity of Vladivostok (Right: 12:56PM, April 18th, 2009, lat=42.844N, lon=130.496E, depth=564km, data by IRIS).

The red arrow indicates the P-wave, the blue indicates the S-wave. Although the figures show vertical ground motions and the S-wave is less visible, it would still be observed in the figure for the natural earthquake, however, no S-wave can be seen in the figure for this event.



Earthquake Location:(click to enlarge)


[Comparison with natural earthquakes - No.2 ]
After the waveforms were low-pass filtered with a corner period of 1s, the S-wave for the natural earthquake becomes distinct, but no S-wave can be seen for this event.
Left: Low-pass filtered waveforms of the event on May 25th, 2009
Right:Low-pass filtered waveforms of the natural earthquake on April 18th, 2009





On the other hand, the ground motion on May 25th, 2009 becomes more distinct after the waveforms are bandpass filtered with a frequency band of 1Hz to 5Hz.
Left: Bandpass filtered waveforms of the event on May 25th, 2009
Right:Bandpass filtered waveforms of the natural earthquake on April 18th, 2009




It is unlikely for a distant M5-class natural earthquake that long-period components are barely observed. (The magnitude of this event was determined by USGS and Japan Meteorological Agency)

[Comparison with the event in Oct. 2006]
Earthquake Observation Center

USGS reported that there occurred a similar event fairly close to the source ofthis event, at 10:35AM, October 9th, 2006 (Japan time). Following is a comparison of waveforms of events both observed at ERI.

The red waveforms indicate the 2006 event, and the blue indicates the 2009 event. Seen that the time difference of both waveforms are the same, it can be said that both events occurred in the same place, and from the similarity of the waveforms, it can be presumed that they hold the same source mechanism.

The numbers at the right end are the maximum amplitudes (x10^-6m/s). It is clear that there is a difference of 3-4times . This makes a difference of 9-16 times if converted into energy.

↓Click to enlarge



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