HR: 0830h
AN: AE21A-1096 [PDF]
TI: COSMIC RAYS AND RUNAWAY ELECTRONS: EVIDENCE FOR ACCELERATION OF ELECTRONS DURING
THUNDERSTORMS
AU: * Lidvansky, A S
EM: lidvansk@sci.lebedev.ru
AF: Institute for Nuclear Research, 60th October Anniversary pr. 7a, Moscow, 117312
Russian Federation
AU: Khaerdinov, N S
EM: khaerdinovs@yandex.ru
AF: Institute for Nuclear Research, 60th October Anniversary pr. 7a, Moscow, 117312
Russian Federation
AU: Petkov, V B
EM: vpetkov@yandex.ru
AF: Institute for Nuclear Research, 60th October Anniversary pr. 7a, Moscow, 117312
Russian Federation
AB:
We present the data on correlations of the intensity of the soft component (10 -30 MeV) of cosmic rays with the local
electric field of the near-earth atmosphere during thunderstorm periods at the Baksan Valley (North Caucasus, 1700 m a. s.
l.). The large-area array for studying the extensive air showers of cosmic rays is used as a particle detector. An electric
field meter of the `electric mill' type is mounted on the roof of the building in the center of this array. The data were
obtained in the summer seasons of 2000--2002. We have observed strong enhancements of the soft component intensity before
some lightning strokes [1]. The largest enhancement detected in the first season demonstrated an exponential growth of
intensity before lightning and was interpreted as a confirmation of runaway electron breakdown mechanism [2]. However, this
event is apparently very rare (a single event for three seasons of observation). The enhancements of a different pattern
(slow events several minutes long) turned out to be much more numerous. Recently, a special experiment was made to estimate
the minimum distance to lightning events [3], and the distances were found to be fairly large (2-5 km). At the same time, the
analysis of the regression curve `intensity versus field' [4] discovers a bump at the field sign that is opposite to the
field sign corresponding to acceleration of electrons (see Fig. 1). It is interpreted as a precipitation of runaway electrons
from the region of the strong field (with the opposite sign) overhead. If this interpretation is true, one can conclude from
these data that (i) Wilson's runaway electrons do exist, (ii) their energy can be pretty high (more than ten MeV), and (iii)
they are not necessarily directly related to lightning events.
Fig. 1. Deviation of the soft component intensity from its mean value versus the near-earth electric field during
thunderstorms. The left-hand side of the plot corresponds to acceleration of electrons near the ground. The bump in the
right-hand side is interpreted as a signature of runaway electrons accelerated and multiplied in the stronger field of
opposite sign at the cloud layer.
REFERENCES
1. Alexeenko, V.V., Khaerdinov, N.S., Lidvansky, A.S., and Petkov, V.B., Transient Variations of Secondary Cosmic Rays due to
Atmospheric Electric Field and Evidence for Pre-Lightning Particle Acceleration, Phys. Lett., A301, 299-306, 2002.
2. Roussel-Dupre, R.A., Gurevich, A.V., Tunnell, T., and Milikh G.M., Kinetic theory of runaway air breakdown, Phys. Rev. E,
49, 2257-2271, 1993.
3. N.S. Khaerdinov, A.S. Lidvansky, V.B. Petkov, Yu.P. Surovetsky, and A.F. Yanin, Estimate of Distance to Lightning Events
Associated with Cosmic Ray Enhancements during Thunderstorms, Proc. 28th ICRC, Tsukuba, Japan, July 31- August 7, 2003,
4165-4168.
4. N.S. Khaerdinov, A.S. Lidvansky, V.B. Petkov, and Yu.P. Surovetsky, Effect of the Disturbed Electric Field of the
Atmosphere on Cosmic Rays: 1. Soft Component, Proc. 28th ICRC, Tsukuba, Japan, July 31- August 7, 2003, pp. 4169-4172.
DE: 3304 Atmospheric electricity
SC: Atmospheric and Space Electricity [AE]
MN: 2003 Fall Meeting