Anomalous Excitation of Schumann Resonances before large earthquakes - - PowerPoint PPT Presentation

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Anomalous Excitation of Schumann Resonances before large earthquakes - - PowerPoint PPT Presentation

Anomalous Excitation of Schumann Resonances before large earthquakes in Japan Jun IZUTSU, Kenji OHTA (Earth Watch - Safety Net Research Center, Chubu University) Masashi HAYAKAWA (University of Electro-Communications) EMSEV-DEMETER Joint


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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Anomalous Excitation of Schumann Resonances before large earthquakes in Japan

Jun IZUTSU, Kenji OHTA

(Earth Watch - Safety Net Research Center, Chubu University)

Masashi HAYAKAWA

(University of Electro-Communications)

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Earth Watch - Safety Net Research Center Chubu University Observation of electromagnetic wave “direct” ULF range (~30Hz) ELF range (223Hz and 17Hz) “indirect” VLF range (Terminator-Time method)

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Observation Network

(Chubu Univ.)

Since 1998

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Induction Coil Antenna

ULF Observation System

1.2m

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Induction Coil Antenna

ULF Observation System

1.2m

Observation of magnetic field (Bx, By, Bz)

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

ULF Observation System

DL-708 Digital Oscilloscope

Block diagram

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

n=1 n=2 n=3 n=4

Observed data

100Hz sampling FFT analyze (N=1024; every 10.24 seconds)

Schumann Resonance

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Observed data

Sonogram Schumann resonance is clearly observed.

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2004 Mid-Niigata Earthquake

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Ohta et al., 2005

10/23 M6.8

2004 Mid-Niigata Earthquake

The intensity at 0.1Hz increased from 10/2 to 10/6. By Goniometer method, we calculate the direction angle

  • f this enhanced EM wave.

The direction angle pointed to the area near the epicenter. Ohta et al. (2005)

Nakatsugawa By 0.1 Hz

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2004 Mid-Niigata Earthquake

Sonogram 2004/10/20 – 2004/10/24 M6.8

n=1 n=2 n=3 n=4 n=1 n=2 n=3 n=4

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2004 Mid-Niigata Earthquake

Sonogram 2004/10/20 18:00 - 24:00

n=3 n=3

Anomalous resonance at 18 Hz Anomalous resonance at 16 Hz

The intensity of Schumann resonance (n=3) increased. Another resonance (18Hz and 16Hz) appeared.

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2004 Mid-Niigata Earthquake

The intensities of the Schumann resonance (n=3) and the anomalous resonance are synchronized. Temporal change of the intensity from 10/19 to 10/27 (1 week)

M6.8

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2007 Noto Earthquake

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2007 Noto Earthquake

Sonogram 2007/03/24 – 2007/03/28 M6.9

n=1 n=2 n=3 n=1 n=2 n=3

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Sonogram 2007/03/25 06:00 - 12:00

2007 Noto Earthquake

M6.9 The intensity of Schumann resonance (n=3) didn’t increase so much. Another resonance (18Hz only) appeared.

n=3 n=3

Anomalous resonance at 18 Hz

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

The intensity of the Schumann resonance (n=3) didn’t increase. The intensity of the anomalous resonance increased just before the earthquake. Temporal change of the intensity from 03/22 to 03/29 (1 week)

M6.8

2007 Noto Earthquake

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2007 Noto Earthquake

Shinojima station was installed in Feb. 2007.

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

2007 Noto Earthquake

M6.9 Sonogram 2007/03/24 – 2007/03/28

No anomalous resonance at Shinojima.

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EMSEV-DEMETER Joint Workshop, Romania, 2008/09/08

Conclusion

The generation mechanism of these anomalous resonances was obscure. ( local problem ? ) We observed anomalous Schumann resonance and another anomalous resonance before 2004 Mid- Niigata earthquake and 2007 Noto earthquake. We installed 3rd ULF station last year. We expect to acquire new information by our new

  • bservation network.