Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini
This report investigates about Seismic-Ionosphere perturbation using Very Low Frequency (VLF) signal Observed in Malaysia. The propagation of VLF signals is between NWC transmitters and receiver at Selangor station. The length of the transmitter receiver -Great Circle Path (TRGCP) is 3000km. The pro...
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my.uitm.ir.818702023-11-12T13:04:44Z https://ir.uitm.edu.my/id/eprint/81870/ Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini Ahmad Kusaini, Nurul Amirah This report investigates about Seismic-Ionosphere perturbation using Very Low Frequency (VLF) signal Observed in Malaysia. The propagation of VLF signals is between NWC transmitters and receiver at Selangor station. The length of the transmitter receiver -Great Circle Path (TRGCP) is 3000km. The propagation path of VLF signal identify the possible ionospheric-perturbations related to the earthquake disaster occurred in Indonesia region within January 2009 - April 2011. Out of seven earthquakes detected within the period only one that show possible evidence is the earthquake at Mentawai Island on 25th October 2010. The magnitude is 7.7 and depth 20.6km. The data was analyzed using three methods (1) average nighttime and daytime amplitude variation (2) terminator time (TT and (3) nighttime fluctuation (NF) methods 2014 Thesis NonPeerReviewed text en https://ir.uitm.edu.my/id/eprint/81870/1/81870.pdf Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini. (2014) Degree thesis, thesis, Universiti Teknologi MARA (UiTM). |
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This report investigates about Seismic-Ionosphere perturbation using Very Low Frequency (VLF) signal Observed in Malaysia. The propagation of VLF signals is between NWC transmitters and receiver at Selangor station. The length of the transmitter receiver -Great Circle Path (TRGCP) is 3000km. The propagation path of VLF signal identify the possible ionospheric-perturbations related to the earthquake disaster occurred in Indonesia region within January 2009 - April 2011. Out of seven earthquakes detected within the period only one that show possible evidence is the earthquake at Mentawai Island on 25th October 2010. The magnitude is 7.7 and depth 20.6km. The data was analyzed using three methods (1) average nighttime and daytime amplitude variation (2) terminator time (TT and (3) nighttime fluctuation (NF) methods |
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Ahmad Kusaini, Nurul Amirah |
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Ahmad Kusaini, Nurul Amirah Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini |
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Ahmad Kusaini, Nurul Amirah |
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Ahmad Kusaini, Nurul Amirah |
title |
Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini |
title_short |
Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini |
title_full |
Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini |
title_fullStr |
Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini |
title_full_unstemmed |
Investigating of VLF signal presecutors for earthquake near Mentawai island / Nurul Amirah Ahmad Kusaini |
title_sort |
investigating of vlf signal presecutors for earthquake near mentawai island / nurul amirah ahmad kusaini |
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2014 |
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https://ir.uitm.edu.my/id/eprint/81870/1/81870.pdf https://ir.uitm.edu.my/id/eprint/81870/ |
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