Termination of Downward‐Oriented Gamma‐Ray Glow by Normal‐Polarity In‐Cloud Discharge Activity

Author:

Wada Y.1ORCID,Wu T.2ORCID,Wang D.2ORCID,Enoto T.34ORCID,Nakazawa K.5ORCID,Morimoto T.6ORCID,Nakamura Y.7,Shinoda T.8,Tsuchiya H.9

Affiliation:

1. Division of Electrical, Electronic and Infocommunications Engineering Graduate School of Engineering Osaka University Suita Osaka Japan

2. Department of Electrical, Electronic and Computer Engineering Gifu University Gifu Gifu Japan

3. Department of Physics Graduate School of Science Kyoto University Kyoto Kyoto Japan

4. Extreme Natural Phenomena RIKEN Hakubi Research Team Cluster for Pioneering Research RIKEN Wako Saitama Japan

5. Kobayashi‐Maskawa Institute for the Origin of Particles and the Universe Nagoya University Nagoya Aichi Japan

6. Faculty of Science and Engineering Kindai University Higashiosaka Osaka Japan

7. Department of Electrical Engineering Kobe City College of Technology Kobe Hyogo Japan

8. Institute for Space‐Earth Environmental Research Nagoya University Nagoya Aichi Japan

9. Nuclear Science and Engineering Center Japan Atomic Energy Agency Tokai‐mura Ibaraki Japan

Abstract

AbstractA gamma‐ray glow, a minute‐lasting burst of high‐energy photons from a thundercloud, was detected by ground‐based apparatus at Kanazawa University, Japan, in a winter thunderstorm on 18 December 2018. The gamma‐ray glow was quenched by a lightning flash within a brief time window of 40 ms. The lightning flash produced several low‐frequency (LF) E‐change pulses that were temporally coincident with the termination of the gamma‐ray glow, and that were located within 0.5 km from the observation site by the Fast Antenna Lightning Mapping Array. The LF pulses had the same polarity as a positive cloud‐to‐ground current and a normal‐polarity in‐cloud current. Since this polarity is against the upward electric field for producing the gamma‐ray glow (accelerating electrons to the ground), we infer that the glow was terminated by a normal‐polarity in‐cloud discharge activity between a middle negative layer and an upper positive layer.

Funder

Japan Society for the Promotion of Science

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

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