Schumann resonance

Schumann resonances may therefore help us to understand these feedback effects.

The Schumann resonances allow to determine the global lightning activity.

Today Schumann resonances are recorded at many separate research stations around the world.

This transit time is what causes the Schumann resonance.

Observations of Schumann resonances have been used to track global lightning activity.

From the very beginning of Schumann resonance studies, it was known that they could be used to monitor global lightning activity.

A new field of interest using Schumann resonances is related to short-term earthquake prediction.

The results of the three studies are somewhat different, but it seems that at least the first two Schumann resonance modes should be detectable.

Since then there has been an increasing interest in Schumann resonances in a wide variety of fields.

Producing 50 lightning events per second, these thunderstorms create the background Schumann resonance signal.

There seem to be no works dedicated to Schumann resonances on Saturn.

To date there has been only one attempt to model Schumann resonances on Jupiter.

This is also known as Schumann resonance.

Measurements of Schumann resonances at only a few stations around the world can monitor the global lightning activity fairly well.

Effects on Schumann resonances have been reported following geomagnetic and ionospheric disturbances.

One of the interesting problems in Schumann resonances studies is determining the lightning source characteristics (the "inverse problem").

Specialized receivers and antennas are needed to detect and record Schumann resonances.

Williams [1992] suggested that global temperature may be monitored with the Schumann resonances.

It appears that only the first Schumann resonance mode might be detectable on Titan.

They'll use this to prove that meteors penetrating the ionosphere have a significant effect on Schumann resonances.

Schumann resonance is due to the space between the surface of the Earth and the conductive ionosphere acting as a waveguide.

These are the Schumann resonances.

Similar results were obtained by Pechony et al. who calculated Schumann resonance fields from satellite lightning data.

The link between Schumann resonance and temperature is lightning flash rate, which increases nonlinearly with temperature.

These resonant modes with their fundamental frequency of f 7.5 Hz are known as Schumann resonances.