High energy radiation from tens of keV to tens of MeV in energy, the transition region from x-rays to gamma rays, has been observed in association with high electric fields in air in many contexts: from the ground, associated with thunderstorms and with individual flashes of natural and rocket-triggered lightning [1, 2, 3, 4, 5, 6, 7, 8] from sparks in the laboratory [9, 10, 11, 12], from Earth orbit in the form of millisecond Terrestrial Gamma-ray Flashes (TGFs) [13,14], and at intermediate altitudes from aircraft and balloons [15,16,17,18,19]. The gamma radiation in all cases is almost certainly bremssfrahlung generated by the collision of accelerated elecfrons with nuclei in the atmosphere. The penefrating gamma-rays can provide a mechanism for coupling between the froposphere, mesosphere, ionosphere and magnetosphere in the form of energetic particles and ionization.