Nw. Watkins et al., A 25-year record of 10 kHz sferics noise in Antarctica: Implications for tropical lightning levels, GEOPHYS R L, 25(23), 1998, pp. 4353-4356
We report measured levels of very low frequency (VLF) radio noise at simila
r to 10 kHz, due to lightning sferics, observed at Halley Station, Antarcti
ca (76 degrees S, 27 degrees W) between 1971 and 1996. The observed VLF noi
se levels at Halley are a product of the thunderstorm source function and t
he transfer function for propagation to the receiver in the waveguide forme
d by the Earth's surface and the ionosphere. Least squares fitting enables
us to confirm the characteristic diurnal, annual and semi-annual periodicit
ies found by the present authors in a separate paper. That method and also
cross correlation of annual averaged 10 kHz VLF power with sunspot number s
hows a similar to 4 dB peak-to-peak fluctuation at the similar to 11-year s
olar cycle period, believed to be due to the influence of EUV flux on the t
he ionospheric D region. Finally we constrain any linear trend to 1.4 +/- 2
.6 dB in 25 years. If a positive trend is present and is interpreted as a c
hange in tropical South American lightning hash rate, it is less than 10 %.