In 2002 Dwyer, along with colleagues from Florida Institute of Technology and the
University of Florida, launched rockets during thunderstorms at a facility now known as the UF/Florida Tech International Center for Lightning Research and Testing (ICLRT) at
Camp Blanding, Florida. Using a heavily shielded instrument containing a
scintillation detector, built by Dwyer and his students, they found that lightning does indeed produce x-rays and that x-ray emission is common for lightning. This research was published in
Science (Dwyer et al. 2003). Since that time, Dwyer and his collaborators have established many key properties of the x-ray emissions from lightning, including the fact that the x-ray emission is produced during the lightning stepping process, has energies up to approximately 1
MeV and the x-rays are produced in the high field regions generated by the leader as it propagates. In 2005 TERA (Thunderstorm Energetic Radiation Array), a 24 detector array, was built to continue measuring x-rays and gamma-rays from lightning and to further study the x-ray characteristics that are associated with thunderstorms. Also, in 2005, Dwyer and collaborators made the surprising discovery that long laboratory sparks in air also generate x-rays similar to lightning, which has since motivated many groups around the world to study the x-ray emissions from sparks. Most recently, Dwyer and his team have built and deployed an x-ray camera at the ICLRT and have made the world's first x-ray images of lightning. Dwyer also has made several important theoretical contributions to the newly developing field of High Energy Atmospheric Physics, including work on runaway electron or
runaway breakdown physics, gamma-ray and radio frequency emissions or atmospheric noise, and lightning initiation. a new discharge mechanism in air, which explains how thunderclouds may generate very large flashes of gamma-rays called
terrestrial gamma-ray flashes (TGFs). This work also showed the importance of
positrons (anti-electrons) for thundercloud electrodynamics. Working with David Smith from UCSC he also helped establish that TGFs originate from deep within our atmosphere and not at high altitudes as had been previously assumed. Indeed, Dwyer and his team observed a ground level TGF at Camp Blanding in 2004. Finally, using BATSE data from the Compton Gamma-ray Observatory, Dwyer and collaborators discovered Terrestrial Electron Beams (TEBs) in the inner magnetosphere, which are generated by the high energy emissions from thunderstorms. ==Achievements==