Imaging of 3 bright terrestrial gamma-ray flashes by the atmosphere-space interactions monitor and their parent thunderstorms

• Published in: Scientific reports Vol. 14; no. 1; p. 6946
• Main Authors: van der Velde, Oscar A., Navarro-González, Javier, Fabró, Ferran, Reglero, Víctor, Connell, Paul, Chanrion, Olivier, López, Jesús A., Montanyà, Joan, Neubert, Torsten, Østgaard, Nikolai
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 23-03-2024; Nature Publishing Group; Nature Portfolio
• Subjects: 639/33; 639/766/419/866; 704/106/35; Atmosphere; Comparative studies; Gamma rays; Humanities and Social Sciences; Lightning; multidisciplinary; Science; Science (multidisciplinary); Thunderstorms; Tropical environment; Tropical environments; Weather
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-024-57229-1

The Atmosphere-Space Interactions Monitor (ASIM) on the International Space Station (ISS) includes an instrument designed to geolocate Terrestrial Gamma-ray Flashes (TGF) produced by thunderstorms. It does so with a coded aperture system shadowing the pixelated Low Energy Detector of the Modular X- and Gamma-ray Sensor (MXGS). Additionally, it locates associated lightning flashes with the Modular Multispectral Imaging Array (MMIA). Here we present 3 bright TGFs with very similar duration, fluency and observation distance. The innovative imaging capabilities allow us to determine the TGF position and correlate the TGF-lightning parent event in time and position simultaneously. The accurate position determination and distance to the observer allow us to perform a comparative study of TGF characteristics. These TGFs were produced in association with lightning flashes below the highest cloud tops of developing to mature convective cells. In one event, GLM (Geostationary Lightning Mapper) cloud flash rates were slowing down after the TGF while negative cloud-to-ground flashes suddenly ceased from 10 to 5 min before the TGF. An 8-stroke (strongest: -93 kA) cloud-to-ground flash occurred 31 s before the TGF. Vertical profiles from the ERA5 reanalysis data suggest TGFs may be produced in variety of tropical environments.