Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS29] Atmospheric Electricity

Sun. May 24, 2015 9:00 AM - 10:45 AM A01 (APA HOTEL&RESORT TOKYO BAY MAKUHARI)

Convener:*Yasuhide Hobara(Graduate School of Information and Engineering Department of Communication Engineering and Informatics, The University of Electro-Communications), Tomoo Ushio(Information and communication engineering department, Osaka University), Chair:Yasuhide Hobara(Graduate School of Information and Engineering Department of Communication Engineering and Informatics, The University of Electro-Communications)

9:00 AM - 9:15 AM

[MIS29-01] Comparison of preliminary breakdown pulses of cloud-to-ground and intracloud lightning flashes

*Yasuhiro AKIYAMA1, Ting Wu1, Gwan KIM1, Hiroshi KIKUCHI1, Tomoo USHIO1, Satoru YOSHIDA2 (1.Osaka University, 2.Meteorological Research Institute)

Keywords:Preliminary breakdown, lightning discharges, EM source location

Using Broadband Observation network for Lightning and Thunderstorm (BOLT) which locates radiation sources in 3D associated with lightning electromagnetic waves in a wide frequency range from 500Hz to 500kHz, we have observed and analyzed Preliminary breakdown (PB) which produces bipolar electric field change waveforms at the beginning of intracloud and cloud-to-ground lightning discharges. We classified PB pulses into +PB and -PB, depending on initial polarity of PB pulses in the physics sign convection and identified 334 +PB pulses and 400 -PB pulses. In this study, we set PB parameters (pulse width, pulse interval, pulse number, total pulse duration and PB initial height, propagation velocity) and analyzed differences between +PB which is at the beginning of intracloud discharges and -PB which is at the beginning of cloud-to-ground discharges. We found that some of +PB's parameters (pulse width, pulse interval, total pulse duration and height) were larger than -PB's parameters. On the other hand, pulse number, velocity were similar with each other. In addition, the results show that radiation sources of +PBs propagate upward while those of -PBs propagate downward or horizontally. In the case of downward propagating -PBs, the ending heights of the propagations are similar to the initial heights of horizontally propagating -PBs. We also use Phased Array Radar (PAR) to make a comparison of radar reflectivity factor and consider the association between thunderstorm's maturity degree and PB parameters.