Key result
Out of 73 early VLF perturbations associated with strong lightning discharges, 64 (84%) were found to be early/slow in nature, occurring mainly during nighttime.
Observational (n=89)
The study characterizes early/slow VLF perturbations associated with lightning discharges at a low latitude station, suggesting daytime events can be used to detect red sprites and elves.
Predominance of early/slow VLF events informs low-latitude monitoring; leaves open validation for daytime sprite detection.
We present here the results of sub-ionospheric VLF perturbations observed on NWC (19.8 kHz) transmitter signal propagating in the Earth-ionosphere waveguide, monitored at our low latitude station Agra. During the period of observation (June-December 2011), we found 89 cases of VLF perturbation, while only 73 cases showing early character associated with strong lightning discharges. Out of 73 events, 64 (~84%) of the early VLF perturbations are found to be early/slow in nature; the remaining 9 events are early/fast. The onset duration of these early/slow VLF perturbations is up to ~ 5 s. A total of 54 observed early events show amplitude change lying between ± 3.0 dB, and phase change ± 12 degree, respectively, and found to occur mainly during nighttime. One of the interesting results we found is that the events with larger recovery time lie far away from the VLF propagation path, while events with smaller duration of recovery are within the ± 50–100 km of signal path. The World Wide Lightning Location Network (WWLLN) data is analysed to find the location of causative lightning and temporal variation. The lightning discharge and associated processes that lead to early VLF events are discussed.
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Uma Pandey (2016) conducted an observational in Sub-ionospheric VLF perturbations (n=89). Lightning discharges was evaluated on Early VLF perturbations. Out of 73 early VLF perturbations associated with strong lightning discharges, 64 (84%) were found to be early/slow in nature, occurring mainly during nighttime.
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