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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.




Measuring Ultra-Low Frequencies


The attohertz (aHz) is an extremely small unit of frequency equal to 10⁻¹⁸ hertz, or one cycle per 10¹⁸ seconds (about 31.7 billion years). This unit is used to describe ultra-low frequency phenomena that occur on cosmic or geological timescales, far beyond everyday human experience.


Attohertz frequencies are relevant in cosmology, astrophysics, and geophysics, where they help scientists study processes that evolve over billions of years. For example, gravitational waves generated by massive cosmic events or the oscillations of the Earth’s magnetic field can be characterized by frequencies in the attohertz range. These waves have enormous wavelengths, often spanning millions or billions of kilometres.


Because the attohertz corresponds to such a long period between cycles, it is mostly used in theoretical research rather than practical applications. Understanding phenomena at this scale gives insight into the fundamental workings of the universe, including the slow evolution of cosmic structures, the expansion of space-time, and the early conditions following the Big Bang.



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