TY - JOUR
T1 - Multiparametric observation of volcanic lightning
T2 - Sakurajima Volcano, Japan
AU - Cimarelli, C.
AU - Alatorre-Ibargüengoitia, M. A.
AU - Aizawa, K.
AU - Yokoo, A.
AU - Díaz-Marina, A.
AU - Iguchi, M.
AU - Dingwell, D. B.
N1 - Funding Information:
C.C. and M.A. acknowledge the financial support of AXA Research Fund through the grant "Risk from Volcanic Ash in the Earth System" and the support of B. Scheu and S. Mueller during high-speed data acquisition and K. Hernández Urbina for the video analysis. The authors are grateful to the SVO staff for logistical support. D.B. Dingwell acknowledges the support of an ERC Advanced Grant EVOKES (247076).
Publisher Copyright:
© 2016. The Authors.
PY - 2016/5/16
Y1 - 2016/5/16
N2 - We recorded volcanic lightning generated by Vulcanian explosions at Sakurajima Volcano using a synchronized multiparametric array. Physical properties of lightning are related to plume dynamics, and associated electromagnetic field variations are revealed by video observations (high speed and normal speed) together with infrasound and high sampling rate magnetotelluric signals. Data show that volcanic lightning at Sakurajima mainly occurs in the plume gas thrust region at a few hundred meters above the crater rim, where the overpressure of the turbulent volcanic jets determines the electrification of particles generating a complex charge structure in the growing plume. Organization of charges may be achieved at later stages when the plume transitions from the jet phase to the convective phase. Comparison with atmospheric sounding and maximum plume height data show that the effect of hydrometeors on flash generation at Sakurajima is negligible and can be more prudently considered as an additional factor contributing to the electrification of volcanic plumes.
AB - We recorded volcanic lightning generated by Vulcanian explosions at Sakurajima Volcano using a synchronized multiparametric array. Physical properties of lightning are related to plume dynamics, and associated electromagnetic field variations are revealed by video observations (high speed and normal speed) together with infrasound and high sampling rate magnetotelluric signals. Data show that volcanic lightning at Sakurajima mainly occurs in the plume gas thrust region at a few hundred meters above the crater rim, where the overpressure of the turbulent volcanic jets determines the electrification of particles generating a complex charge structure in the growing plume. Organization of charges may be achieved at later stages when the plume transitions from the jet phase to the convective phase. Comparison with atmospheric sounding and maximum plume height data show that the effect of hydrometeors on flash generation at Sakurajima is negligible and can be more prudently considered as an additional factor contributing to the electrification of volcanic plumes.
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U2 - 10.1002/2015GL067445
DO - 10.1002/2015GL067445
M3 - Article
AN - SCOPUS:84962448286
SN - 0094-8276
VL - 43
SP - 4221
EP - 4228
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 9
ER -