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Auroral chorus

Geomagnetic phenomenon

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Through Electromagnetic radiation, Ionosphere and Speed of sound

The electromagnetic waves are a type of natural radio waves, vibrations of electric and magnetic energy occurring at the same frequency as sound.

Detection

Auroral chorus can be detected primarily around the magnetic equator, specifically in two distinct frequency bands, one above the equatorial half gyro-frequency and one below it. The gyro-frequency ranges from 0.6 kHz to about 1.6 kHz. Distinguishable on high resolution wideband spectrographs, the wave amplitude grows linearly then switches to non-linear. Demonstrating a peak distribution near dawn, the auroral chorus is most detectable via ELF/VLF Radio receivers in the middle latitude around 30-60 degrees N. The most numerous recordings of the auroral chorus has been by the Iowa Plasma Wave Group. They have released many audio interpretations of chorus recordings online along with spectrograph measurements.

Historically, the sounds have been associated with spiritual events by Inuit in Canada who regularly experienced auroral chorus on cold, windless nights.

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