Journal of Geophysical Research Atmospheres, volume 123, issue 13, pages 6864-6879
Gamma Ray Showers Observed at Ground Level in Coincidence With Downward Lightning Leaders
R. U. ABBASI
1
,
T. Abu-Zayyad
1
,
M. ALLEN
1
,
E. BARCIKOWSKI
1
,
J. W. Belz
1
,
D. R. Bergman
1
,
S. A. BLAKE
1
,
M. Byrne
1
,
R. CADY
1
,
B. G. CHEON
2
,
J. CHIBA
3
,
M. CHIKAWA
4
,
T. Fujii
5
,
M. FUkUSHIMA
5, 6
,
G. Furlich
1
,
T. Goto
7
,
W. HANLON
1
,
Y. Hayashi
7
,
N. HAYASHIDA
8
,
K. Hibino
8
,
K. HONDA
9
,
D. IKEDA
5
,
N. INOUE
10
,
T. Ishii
9
,
H. Ito
11
,
D. Ivanov
1
,
S. Jeong
12
,
C. C. H. Jui
1
,
K. KADOTA
13
,
F. KAKIMOTO
14
,
O. Kalashev
15
,
K. KASAHARA
16
,
H. Kawai
17
,
S. KAWAKAMI
7
,
K. Kawata
5
,
E. Kido
5
,
H. B. Kim
2
,
J H Kim
18
,
S S Kishigami
7
,
Paul R. Krehbiel
19
,
V. KUZMIN
15
,
Y. J. Kwon
20
,
J. Lan
1
,
R Levon
1
,
J. P. LUNDQUIST
1
,
K Machida
9
,
K. MARTENS
6
,
T Matuyama
7
,
J. N. MATTHEWS
1
,
M. MINAMINO
7
,
K. Mukai
9
,
I. MYERS
1
,
S. Nagataki
11
,
R. Nakamura
21
,
T. Nakamura
22
,
T. NONAKA
5
,
S. Ogio
7
,
M. OHNISHI
5
,
H. OHOKA
5
,
K. Oki
5
,
T. Okuda
23
,
Masaomi Ono
24
,
M. Ono
24
,
R. ONOGI
7
,
A. OSHIMA
25
,
S. OZAWA
16
,
I. H. PARK
12
,
M. S. Pshirkov
13, 26
,
J. Remington
1
,
W Rison
19
,
D Rodeheffer
19
,
D. C. RODRIGUEZ
1
,
G. Rubtsov
15
,
D. RYU
18
,
H. Sagawa
5
,
K. SAITO
5
,
N. SAKAKI
5
,
N. SAKURAI
7
,
T. Seki
21
,
K. SEKINO
5
,
P. D. SHAH
1
,
F. SHIBATA
9
,
T Shibata
5
,
H. SHIMODAIRA
5
,
B. K. SHIN
7
,
H. S. Shin
5
,
J. D. Smith
1
,
Pierre Sokolsky
1
,
P. Sokolsky
1
,
R. W. Springer
1
,
B. T. Stokes
1
,
T. A. STROMAN
1
,
H. Takai
27
,
M. Takeda
5
,
R. TAKEISHI
5
,
A. TAKETA
28
,
M. TAKITA
5
,
Y. Tameda
29
,
H Tanaka
7
,
H. Tanaka
7
,
K Tanaka
30
,
Masayuki Tanaka
31
,
Ronald J Thomas
19
,
S. B. Thomas
1
,
G. B. THOMSON
1
,
P. TINYAKOV
15, 32
,
I. Tkachev
15
,
H. Tokuno
14
,
T. TOMIDA
21
,
S. Troitsky
15
,
Y. TSUNESADA
7
,
Y. UCHIHORI
33
,
S. UDO
8
,
F. URBAN
32
,
G. Vasiloff
1
,
T. Wong
1
,
M. Yamamoto
21
,
R. Yamane
7
,
H. Yamaoka
31
,
K. Yamazaki
28
,
J. Yang
34
,
K. Yashiro
3
,
Y. Yoneda
7
,
S. YOSHIDA
17
,
H. YOSHII
35
,
Z. ZUNDEL
1
2
4
Department of PhysicsKinki University Higashi‐osaka Japan
|
Publication type: Journal Article
Publication date: 2018-05-17
scimago Q1
SJR: 1.710
CiteScore: 7.3
Impact factor: 3.8
ISSN: 2169897X, 21698996
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Geophysics
Abstract
Bursts of gamma ray showers have been observed in coincidence with downward propagating negative leaders in lightning flashes by the Telescope Array Surface Detector (TASD). The TASD is a 700~square kilometer cosmic ray observatory located in southwestern Utah, U.S.A. In data collected between 2014 and 2016, correlated observations showing the structure and temporal development of three shower-producing flashes were obtained with a 3D lightning mapping array, and electric field change measurements were obtained for an additional seven flashes, in both cases co-located with the TASD. National Lightning Detection Network (NLDN) information was also used throughout. The showers arrived in a sequence of 2--5 short-duration ($\le$10~$\mu$s) bursts over time intervals of several hundred microseconds, and originated at an altitude of $\simeq$3--5 kilometers above ground level during the first 1--2 ms of downward negative leader breakdown at the beginning of cloud-to-ground lightning flashes. The shower footprints, associated waveforms and the effect of atmospheric propagation indicate that the showers consist primarily of downward-beamed gamma radiation. This has been supported by GEANT simulation studies, which indicate primary source fluxes of $\simeq$$10^{12}$--$10^{14}$ photons for $16^{\circ}$ half-angle beams. We conclude that the showers are terrestrial gamma-ray flashes (TGFs), similar to those observed by satellites, but that the ground-based observations are more representative of the temporal source activity and are also more sensitive than satellite observations, which detect only the most powerful TGFs.
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