Changes of the Geomagnetic Signals Linked to Tohoku Earthquake on March 11th 2011

International Journal of Technology

TetiZubaidah¹  BulkisKanata¹  CiptaRamadhani²  BudiIrmawati³ 

[1] Electrical Engineering Department, Faculty of Engineering, Mataram University, Jl.Majapahit 62, Mataram 83125, Indonesia;Electrical Engineering Department, Faculty of Engineering, Mataram University, Jl. Majapahit 62, Mataram 83125, Indonesia;Informatics Engineering Study Program, Faculty of Engineering, Mataram University, Jl.Majapahit 62, Mataram 83125, Indonesia;

关键词: Earthquake, Geomagnetic, Polarization, psd;   

DOI  :  10.14716/ijtech.v5i3.1315

来源: DOAJ

【 摘 要 】

The geomagnetic fields in the atmosphere can be affected by phenomena in the Earth, so that changes of geomagnetic intensity might be used as an indicator of earthquake occurrences. Variations of geomagnetic data have been analyzed in association with the Tohoku Earthquake on March 11th 2011. The Geomagnetic data have been derived from Memambetsu (MMB), Kakioka (KAK) and Kanoya (KNY) Observatories, which are INTERMAGNET observatories. The analysis was performed by calculating the power spectral density (psd) of the ULF signal of Z and H components and then polarizations are observed by comparing the psd of Z and of H. The results showed the difference psd of Z and of H between the KAK observatory (the nearest position to the epicenter) with MMB and KNY (at some greater distance from the epicenter) is quite significant, which can be observed over a period of 10 days before the earthquake occurrence. The polarizations of Z/H in KAK indicate a highest change of intensity which occurred at 18 days prior to the earthquake.

【 授权许可】

Unknown