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Understanding Low-Frequency Oscillations

The millihertz (mHz) is a unit of frequency equal to 10⁻³ hertz, meaning one cycle occurs every 1,000 seconds or roughly 16.7 minutes. This low-frequency range is important in fields such as seismology, astrophysics, and geophysics, where it describes slow, periodic events that unfold over minutes to hours.

In astrophysics, millihertz frequencies are commonly observed in solar oscillations and stellar pulsations, providing key information about the internal structure and dynamics of stars. These oscillations help scientists understand energy transport, magnetic activity, and the life cycles of stars.

In geophysics, millihertz frequencies correspond to long-period seismic waves generated by earthquakes or volcanic activity. These waves travel long distances through the Earth’s interior and can reveal valuable data about its composition and structure.

Additionally, millihertz frequencies are relevant in oceanography and atmospheric science for studying tides, slow atmospheric waves, and other natural cycles that influence climate and weather patterns.

Because millihertz oscillations have relatively long periods and wavelengths, they allow researchers to probe processes that develop over extended timeframes and large spatial scales, bridging the gap between faster waves and ultra-low-frequency phenomena.

The Scale of Extremely Low Frequency and Astrophysical Waves

A gigametre (Gm) is equal to 1,000,000,000 metres (10⁹ m) and is used to describe extraordinarily long wavelengths found primarily in the extremely low frequency (ELF) band and in astrophysical phenomena. These wavelengths correspond to frequencies in the millihertz to microhertz range, far below typical human-made radio communications. Gigametre-scale wavelengths are associated with very slow oscillations in space plasmas, planetary magnetospheres, and cosmic radio waves.

For example, a frequency of 1 microhertz (10⁻⁶ Hz) corresponds to a wavelength of about 300 million kilometres (300 Gm), which is roughly twice the distance from the Earth to the Sun. Such enormous wavelengths are significant in studying solar-terrestrial interactions, long-period gravitational waves, and other phenomena in astrophysics and cosmology.

Although gigametre wavelengths are not practical for terrestrial communications, they help scientists understand the large-scale electromagnetic environment of the solar system and beyond. Using the gigametre unit allows researchers to quantify these immense scales and analyze signals and waves that influence planetary environments, space weather, and the interstellar medium.