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Somehow, he explained, lightning discharges in the lower atmosphere are having effects in the upper atmosphere.
Lightning discharges occur when the accumulated electric charge becomes sufficiently large.
On the early Earth much more energy was available in ultraviolet light than from lightning discharges.
The surface and the atmosphere form a giant battery, as the lightning discharges of thunderstorms demonstrate.
These electromagnetic waves originate during lightning discharges and are usually in the frequency range of 300 to 30,000 hertz.
In recent years it has become clear that lightning can be artificially initiated, or triggered, in clouds that would not normally produce natural lightning discharges.
The other possible energy source for the IAR excitation is related to lightning discharges.
The LLS detects mainly cloud to ground (CG) and ground to cloud (GC) lightning discharges.
Meshed areas indicate zones of undetectable lightning discharges with absolute peak currents below 10 kA.
The natural sources in this frequency range are mainly due to lightning discharges.
The lightning discharges located ±50 100 km around the receiver and/or transmitter have also been attributed to narrow-angle forward scattering, as the area with perturbed electron density due to lightning discharges would overlap the transmitter or receiver.
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