ELF and VLF radio waves

The global electrical circuit: A review

Aliasing of the Schumann resonance background signal by sprite-associated Q-bursts

We present the results of statistical R/S analysis of natural electromagnetic noise in the frequency range of Schumann resonance. The Hurst exponent was derived for the records of two horizontal magnetic antennas performed at the Negev desert, Israel. Analysis shows that ELF radio noise is an anti-persistent random process. Temporal variations of the R/S ratio contain diurnal and slower variations probably indicating changes in the global lightning rate.

https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1999GL000015

Hurst exponent derived for natural terrestrial radio noise in Schumann resonance band

Schumann resonance transients which propagate around the globe can potentially generate a correlated background in widely separated gravitational wave detectors. We show that due to the distribution of lightning hotspots around the globe these transients have characteristic time lags, and this feature can be useful to further suppress such a background, especially in searches of the stochastic gravitational-wave background. A brief review of the corresponding literature on Schumann resonances and lightnings is also given.

Schumann resonance transients and the search for gravitational waves

Two distinct measures of the Earth's Schumann resonances-the background and the transients--are studied through comparisons at the mesoscale and at the continental scale. A rough proportionality is shown between the far more abundant afternoon lightning activity and the larger positive mesoscale discharges that make sprites and simultaneously ring the Earth-ionosphere cavity to levels higher than the integration of all other lightnings.

The Relationship Between the Background and Transient Signals in Schumann Resonances

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The Relationship Between the Background and Transient Signals in Schumann Resonances