Tropospheric scatter
Tropospheric scatter, also known as troposcatter, is a radio communication method that enables beyond-line-of-sight transmission of microwave signals over distances up to approximately 1000 kilometers by exploiting the scattering of waves off refractive index irregularities in the troposphere, the lowest atmospheric layer extending roughly 2–5 kilometers above the Earth's surface.[1] This technique relies on directing high-power signals slightly above the horizon, where a fraction scatters back to receiving antennas via a common volume of turbulent air, though it incurs substantial path losses necessitating large parabolic antennas, amplifiers, and sensitive receivers.[1][2] Operating primarily in frequency bands above 500 MHz, such as 2–5 GHz, troposcatter provided reliable, high-capacity links for voice, data, and telemetry in remote or infrastructure-poor regions where alternatives like cables or satellites were impractical.[1][2] Developed in the early 1950s amid Cold War demands for secure over-the-horizon military communications, it underpinned systems like the U.S. Air Force's Pole Vault network connecting radar sites across Greenland and eastern Canada, and later the White Alice array in Alaska for strategic defense.[3] Despite challenges including signal fading from atmospheric variations and the need for site-specific engineering, troposcatter's jam-resistant qualities and independence from vulnerable infrastructure made it a cornerstone of NATO and U.S. tactical deployments, with modern iterations adapting digital modulation for contested environments as satellite alternatives face jamming threats.[4][5]