VLF/LF Amplitude Perturbations before Tuscany Earthquakes, 2013
- 1 St. Xavier’s College, Kathmandu, Nepal
- 2 St. Xavier’s College, Kathmandu, Nepal
- 3 St. Xavier’s College, Kathmandu, Nepal
- 4 St. Xavier’s College, Kathmandu, Nepal
- 5 St. Xavier’s College, Kathmandu, Nepal
- 6 Nepalese Center for Research in Physical Sciences (NCRPS), Kathmandu, Nepal
Abstract
The US Navy VLF/LF Transmitter’s NSY signal (45.9 kHz) transmitted from Niscemi, Sicily, Italy, and received at the Kiel Long Wave Monitor, Germany, was analyzed for the period of two months, May and June (EQ-month) of 2013. There were 12 earthquakes of magnitude greater than 4 that hit Italy in these two months, of which the earthquake of 21 st June having magnitude of 5.2 and a shallow focal depth of 5 km was the major one. We studied the earthquake of 21 st of June 2013, which struck Tuscany, Central Italy, (44.1713 ° N and 10.2082 ° E) at 10:33 UT, and also analyzed the effects of this earthquake on the sub-ionos- pheric VLF/LF signals. In addition, we also studied another earthquake, of magnitude 4.9, which hit the same place at 14:40 UT on 30 th of June and had shallow focal depth of 10 km. We assessed the data using terminator time (TT) method and night time fluctuation method and found unusual changes in VLF/LF amplitudes/phases. Analysis of trend, night time dispersion, and night time fluctuation was also carried and several anomalies were detected. Most ionospheric perturbations in these parameters were found in the month of June, from few days to few weeks prior to the earthquakes. Moreover, we filtered the possible effects due to geomagnetic storms, auroras, and solar activities using parameters like Dst index, AE index, and Kp index for analyzing the geomagnetic effects, and Bz (sigma) index, sunspot numbers, and solar index F10.7 for analyzing the solar activities for the confirmation of anomalies as precursors.
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