Tsunami-driven ionospheric perturbations associated with the 2011 Tohoku earthquake as detected by subionospheric VLF signals

The subionospheric data from a Japanese very low frequency/low frequency (VLF/LF) receiving station at Moshiri, Hokkaido, are used to detect the response of the lower ionosphere to the tsunami triggered by the 2011 Tohoku earthquake. Disturbances in the phase and amplitude of VLF signals propagating...

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Veröffentlicht in:Geomatics, natural hazards and risk natural hazards and risk, 2014-10, Vol.5 (4), p.285-292
Hauptverfasser: Rozhnoi, A., Solovieva, M., Hayakawa, M., Yamaguchi, H., Hobara, Y., Levin, B., Fedun, V.
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container_end_page 292
container_issue 4
container_start_page 285
container_title Geomatics, natural hazards and risk
container_volume 5
creator Rozhnoi, A.
Solovieva, M.
Hayakawa, M.
Yamaguchi, H.
Hobara, Y.
Levin, B.
Fedun, V.
description The subionospheric data from a Japanese very low frequency/low frequency (VLF/LF) receiving station at Moshiri, Hokkaido, are used to detect the response of the lower ionosphere to the tsunami triggered by the 2011 Tohoku earthquake. Disturbances in the phase and amplitude of VLF signals propagating from the transmitter in Hawaiian Islands are observed during the tsunami wave passage, and these effects in the ionosphere are compared to the in situ sea-level global positioning system (GPS) measurements near Japan. The frequency of the maximum spectral amplitude both for the VLF and GPS data is found to be in the range of periods of 8-50 min, which is likely to correspond to the period of the internal gravity waves generated by the tsunami.
doi_str_mv 10.1080/19475705.2014.888100
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subjects Amplitudes
Global Positioning System
Receiving
Risk
Seismic phenomena
Tsunamis
VLF
Wave propagation
title Tsunami-driven ionospheric perturbations associated with the 2011 Tohoku earthquake as detected by subionospheric VLF signals
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