The initial stage processes of rocket-and-wire triggered lightning as observed by VHF interferometry

被引:33
作者
Yoshida, S. [1 ]
Biagi, C. J. [2 ]
Rakov, V. A. [2 ]
Hill, J. D. [2 ]
Stapleton, M. V. [2 ]
Jordan, D. M. [2 ]
Uman, M. A. [2 ]
Morimoto, T. [1 ]
Ushio, T. [1 ]
Kawasaki, Z. -I. [1 ,3 ]
Akita, M. [1 ]
机构
[1] Osaka Univ, Dept Informat & Commun Technol, Suita, Osaka 5650871, Japan
[2] Univ Florida, Dept Elect & Comp Engn, Gainesville, FL USA
[3] Egypt Japan Univ Sci & Technol, Alexandria, Egypt
基金
美国国家科学基金会;
关键词
INTERNATIONAL PROGRAM TRIP; TRANSMISSION-LINE MODEL; ELECTROMAGNETIC-RADIATION; RETURN STROKES; M COMPONENTS; DISCHARGES; FLASHES; CLOUD; CURRENTS; LEADERS;
D O I
10.1029/2012JD017657
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We examine VHF interferometric images, channel-base currents, and broadband electric field waveforms of the initial stage (IS) in two rocket-and-wire triggered lightning flashes. Two types of negative leaders, termed "long-duration" and "short-duration" leaders, were imaged by the VHF interferometers during the IS of the two flashes. There were three leaders that had relatively long durations of more than a few milliseconds. These three leaders were not accompanied by a significant change of channel-base current during their early stages of development, indicating that they corresponded to intracloud (IC) discharges that were not connected to the grounded triggered-lightning channel. Two of these three leaders eventually connected to the triggered-lightning channel and initiated initial continuous current (ICC) pulses. The third long-duration leader apparently developed from the vicinity of an isolated negative charge region toward an upper-level positive charge region and toward a branch of the grounded channel; it served to bridge the positive charge region and the triggered-lightning channel, resulting in the opposite polarity portion of the bipolar ICC. The short-duration negative leaders had durations of some hundreds of microseconds. These negative leaders apparently recoiled along the conductive channels created by branches of the upward positive leader (UPL); they initiated ICC pulses when the grounded channel was sufficiently conductive. It follows that ICC pulses can be initiated either by recoil leaders or via interception of separate in-cloud leaders by a grounded current-carrying channel.
引用
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页数:12
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