The signature of the 2011 Tohoku mega earthquake on the geomagnetic field measurements in Japan | ||
| NRIAG Journal of Astronomy and Geophysics | ||
| Volume 2, Issue 2, December 2013, Pages 185-195 PDF (7.16 M) | ||
| DOI: 10.1016/j.nrjag.2013.08.001 | ||
| Authors | ||
| E.M. Takla; K. Yumoto; S. Okano; T. Uozumi; S. Abe | ||
| Abstract | ||
| On 11 March 2011 at 05:46:23 UTC, a mega earthquake (EQ) with magnitude (Mw) 9.0 [The 2011 Tohoku Earthquake] occurred at a depth of about 24 km near the East coast of Honshu Island, Japan as a result of a thrust faulting on or near the subduction plate boundary between the Pacific and North American plates. Geomagnetic data from MAGDAS and Geospatial Information Authority of Japan (GSI) networks have been analyzed to examine the signature of the 2011 Tohoku earthquake on the geomagnetic field measurements in Japan. Results of data analysis indicate about 5 nT increase in the total geomagnetic field intensity in the vicinity of the epicenter of 2011Tohoku EQ compared with other reference stations. Moreover, the annual range of the Z-component daily variations tends to decrease near the epicenter before the occurrence of the Tohoku EQ. Concerning the ULF emissions; the Pc 3 amplitude ratio (ZPc3/HPc3) near the epicenter at the Onagawa [ONW] station showed a good correlation with other remote reference stations before the Tohoku EQ but it started to decrease with no correlation to other stations a few weeks before the 2011 Tohoku EQ. On the other hand, the Pc 3 amplitude ratio at ONW station showed a clear anti-correlation compared with reference stations after the 2011 Tohoku EQ. | ||
| Keywords | ||
| Geomagnetic variations; ULF signal; Piezomagnetic effect; Crustal stress; 2011 Tohoku earthquake | ||
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