The field guide · Earth

Schumann resonance frequencies, explained.

The first Schumann resonance is approximately 7.8 Hz. Other broad modes occur near 14, 20, 26 and 33 Hz. These values describe oscillation rates; amplitude and spectral power describe different properties of the recorded signal.

Illustrative spectrum with broad peaks near 7.8, 14, 20, 26 and 33 hertz; the vertical axis is relative amplitude.Open chart at full size ↗
Schumann Pulse teaching figure · authored mathematical peaks, normalized amplitude. Not observed data; approximate mode positions are explained in the text.

What does a hertz measure?

One hertz means one cycle per second. A frequency near 7.8 Hz therefore describes a field oscillating roughly eight times each second. It does not describe how strong the field is, how much energy a person has, or how quickly the whole planet rotates.

A useful reading habit is to say both the number and the unit aloud. “Eight hertz” and “eight relative units” may look similar in a headline, but they answer different questions.

The first five modes

The rounded values below are orientation points, not a specification that every observation must match. A four-year study using Sierra Nevada magnetometers examines regular variations rather than treating the modes as fixed constants.

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Mode Approximate frequency How to interpret it
First 7.8 Hz The lowest prominent resonance band
Second 14 Hz A higher resonant mode
Third 20 Hz A separate band, not a jump of the first mode
Fourth 26 Hz Another higher mode
Fifth 33 Hz A higher-frequency band in the same system
Illustrative spectrum with broad peaks near 7.8, 14, 20, 26 and 33 hertz; the vertical axis is relative amplitude.Open chart at full size ↗
Schumann Pulse teaching figure · authored mathematical peaks, normalized amplitude. Not observed data; approximate mode positions are explained in the text.

This teaching spectrum uses smooth mathematical peaks. Its vertical scale is normalized and has no physical calibration. It is not a station measurement or a model fitted to an observed day.

Frequency is not amplitude

Imagine a peak centered near 8 Hz becoming twice as tall while staying in the same place. Its plotted amplitude has increased; its central frequency has not doubled. Now imagine that same peak moving slightly sideways without becoming taller. That illustrates a frequency change.

A published plot may show electric field, magnetic field, amplitude spectral density, power spectral density or a provider-specific index. Those quantities cannot be substituted for one another. Compare values only after checking the axis and the processing method.

Why “Earth’s frequency rose to 40” is incomplete

Before accepting that statement, ask: 40 what? Which sensor? Which mode? At what time? Was the number read from a frequency axis or an amplitude label? A bright feature reaching 40 Hz on a spectrogram may cover a wide frequency range; it does not demonstrate that the lowest resonance has become 40 Hz.

The Nagycenk display documentation is a useful real example: it describes dynamic spectra and separately extracted mode amplitudes and frequencies. These are different views of the observations, not interchangeable names for one number.

Can you hear 7.83 Hz?

A plotted electromagnetic frequency is not automatically an audio recording. Audio advertised with this number may be synthesized or use modulation. It should not be presented as direct evidence of what a ground observatory measured. Our guides explain environmental measurements, not audio treatments.

Why the unit is called hertz

The unit honours Heinrich Hertz and his electromagnetic-wave experiments. It measures cycles per second, independently of a signal’s strength.

Sources

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