The Far Ultra-violet Background

The diffuse far-ultraviolet (FUV) background has received considerable attention from astronomers since the 1970s The initial impetus came from the hope of detecting UV radiation from the hot intergalactic medium. The central importance of the FUV background to the physics (heating and ionization) of the diffuse atomic phases motivated the next generation of experiments. The consensus view is that the diffuse FUV emission at high latitudes has three components: stellar FUV reflected by dust grains (diffuse galactic light or DGL), FUV from other galaxies and the intergalactic medium (extra-galactic background light or EBL) and a component of unknown origin (and referred to as the offset component). During the 1980s, there was some discussion that decaying dark matter particles produced FUV radiation. In this paper I investigate production of FUV photons by conventional sources: line emission from Galactic Hot Ionized Medium, two-photon emission from the Galactic Warm Ionized Medium and low-velocity shocks, and Lyman-beta fluorescence of hydrogen at several locales in the Solar System (the interplanetary medium, the exosphere and the thermosphere of Earth). I conclude that two thirds and arguably all of the offset component can be explained by the sum of the radiation from the processes listed above.

Automated summary

The diffuse far-ultraviolet (FUV) background has been a subject of interest to astronomers since the 1970s. It plays a central role in the physics of diffuse atomic phases. The high latitude diffuse FUV emission is believed to have three components: stellar FUV reflected by dust grains, FUV from other galaxies and the intergalactic medium, and an unknown offset component. This paper investigates the production of FUV photons by conventional sources and concludes that most, if not all, of the offset component can be explained by the radiation from these sources.