| Literature DB >> 26986281 |
D Umemoto1, H Tsuchiya2,3, T Enoto2,4, S Yamada5, T Yuasa2, M Kawaharada6, T Kitaguchi7, K Nakazawa1, M Kokubun6, H Kato2, M Okano2, T Tamagawa2, K Makishima1,8.
Abstract
Thunderclouds can produce bremsstrahlung gamma-ray emission, and sometimes even positrons. At 00:27:00 (UT) on 13 January 2012, an intense burst of gamma rays from a thundercloud was detected by the GROWTH experiment, located in Japan, facing the Sea of Japan. The event started with a sharp gamma-ray flash with a duration of <300 ms coincident with an intracloud discharge, followed by a decaying longer gamma-ray emission lasting for ∼60 s. The spectrum of this prolonged emission reached ∼10 MeV, and contained a distinct line emission at 508±3(stat.)±5(sys.) keV, to be identified with an electron-positron annihilation line. The line was narrow within the instrumental energy resolution (∼80keV), and contained 520±50 photons which amounted to ∼10% of the total signal photons of 5340±190 detected over 0.1-10 MeV. As a result, the line equivalent width reached 280±40 keV, which implies a nontrivial result. The result suggests that a downward positron beam produced both the continuum and the line photons.Entities:
Year: 2016 PMID: 26986281 DOI: 10.1103/PhysRevE.93.021201
Source DB: PubMed Journal: Phys Rev E ISSN: 2470-0045 Impact factor: 2.529