Convert wavelength in hectometres to microhertz [µHz] Online | Free frequency-wavelength Converter

Describing Very Low Frequency Radio Waves

A hectometre (hm) is a unit of length equal to 100 metres, and it is used to describe very long wavelengths in the Very Low Frequency (VLF) and Low Frequency (LF) bands of the electromagnetic spectrum. Wavelengths in the hectometre range correspond to frequencies between approximately 3 kHz and 3 MHz. These long wavelengths are typically used for maritime navigation, military submarine communication, AM radio broadcasting, and time signal transmissions.

For example, a signal at 300 kHz has a wavelength of 1 kilometre, or 10 hectometres, and a signal at 1 MHz corresponds to 3 hectometres. These long wavelengths have the unique ability to travel long distances and penetrate water and the ground, which is why they are used in submarine communications and emergency broadcast systems.

Using hectometres to express wavelength offers a practical scale for understanding wave propagation over great distances. It also aids in antenna design, where very large antennas—often hundreds of metres long—are needed to efficiently transmit or receive these frequencies. Understanding wavelength in hectometres is important in geophysics, radio astronomy, and large-scale communications infrastructure.

Exploring Ultra-Slow Periodic Phenomena

The microhertz (µHz) is a unit of frequency equal to 10⁻⁶ hertz, meaning one cycle occurs every 1,000,000 seconds or approximately 11.6 days. This very low frequency range is significant in astrophysics, geophysics, and various scientific disciplines that study slow, periodic phenomena spanning days to weeks.

In astrophysics, microhertz frequencies are important for observing oscillations in stars, including our Sun. Solar oscillations, known as helioseismic waves, occur in the microhertz range and provide valuable insights into the Sun’s internal structure and dynamics. These oscillations help scientists understand stellar processes, energy transport, and magnetic activity.

On Earth, microhertz frequencies correspond to slow geophysical processes such as tectonic plate motions, long-period seismic waves, and atmospheric tides. These phenomena unfold over days and influence climate and geological activity.

Because microhertz frequencies represent slow oscillations with very long wavelengths (thousands to millions of kilometres), they provide a unique window into dynamic processes that evolve over extended timeframes. Studying microhertz waves allows researchers to connect daily to weekly timescales with broader natural cycles.