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Understanding Extremely Low Frequency Waves


A kilometre (km) is a unit of length equal to 1,000 metres, and in the context of electromagnetic waves, it is used to describe extremely long wavelengths, typically in the Very Low Frequency (VLF) and Extremely Low Frequency (ELF) ranges. These wavelengths correspond to very low frequencies, usually below 300 kHz, and are commonly used in long-distance radio communication, submarine communication, navigation systems, and geophysical research.


For instance, a frequency of 30 kHz has a wavelength of 10 km, while 3 kHz corresponds to a wavelength of 100 km. These long wavelengths can travel great distances, penetrate seawater, and diffuse around obstacles, making them ideal for communication with submerged submarines and in areas where traditional signals cannot reach. ELF waves, with wavelengths of hundreds to thousands of kilometres, are also used in Earth monitoring, such as detecting seismic or lightning activity.


Using kilometres to measure wavelength allows scientists and engineers to understand and design systems for global communication and natural signal monitoring. Although challenging to generate and detect, kilometre-scale wavelengths play a vital role in specialized but critical applications.




The Realm of Extremely Slow Oscillations


The nanohertz (nHz) is a unit of frequency equal to 10โปโน hertz, meaning one cycle occurs every 1 billion secondsโ€”about 31.7 years. This incredibly low frequency is important in fields like astrophysics, cosmology, and geophysics, where slow periodic phenomena unfold over decades to centuries.


Nanohertz frequencies are often associated with gravitational waves produced by supermassive black hole binaries orbiting each other over many years. These ultra-low-frequency waves have immense wavelengths, spanning light-years across space. Pulsar timing arrays, which monitor the precise arrival times of pulsar signals, are used to detect such nanohertz gravitational waves, offering insights into galaxy evolution and cosmic structure.


On Earth, nanohertz frequencies can describe long-term oscillations in the geomagnetic field or climate cycles. Studying these slow frequencies helps scientists understand gradual changes in planetary environments and the universe.


Although nanohertz waves are far below everyday human perception and technological applications, they are critical for unraveling the universe's slowest dynamics. Using nanohertz as a unit helps researchers quantify and analyze these grand-scale processes, linking time scales from decades to cosmic evolution.





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