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Global diagnostics of the ionospheric perturbations related to the seismic activity using the VLF radio signals collected on the DEMETER satellite

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Figure

Fig. 1. An example of registration in the 10–20 kHz range during one orbit of the satellite on 29 December 2004
Fig. 2. The stars indicate the location of the powerful VLF transmitters in the eastern hemisphere
Fig. 4. The averaged SNR distribution during two months of ob-servation for the NWC transmitter (F=19.8 kHz)
Fig. 7. Averaged SNR distributions for the DFY transmitter (16.56 kHz): (a) the same as in Fig
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