Characteristics of lightning leader propagation and ground attachment

被引:37
作者
Jiang, Rubin [1 ,2 ]
Qie, Xiushu [1 ,2 ]
Wang, Zhichao [1 ]
Zhang, Hongbo [1 ]
Lu, Gaopeng [1 ,2 ]
Sun, Zhuling [1 ]
Liu, Mingyuan [1 ]
Li, Xun [3 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, Key Lab Middle Atmosphere & Global Environm Obser, Beijing, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteorl, Nanjing, Jiangsu, Peoples R China
[3] Chengdu Univ Informat Technol, Col Meteorol Observat, Chengdu, Peoples R China
基金
中国国家自然科学基金;
关键词
RETURN STROKES; MILLISECOND-SCALE; FLASHES; TERMINATIONS; INTENSITY; DISCHARGE; FEATURES; SYSTEM; STRIKE; PEAK;
D O I
10.1002/2015JD023519
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The grounding process and the associated leader behavior were analyzed by using high-speed video record and time-correlated electric field change for 37 natural negative cloud-to-ground flashes. Weak luminous grounded channel was recognized below the downward leader tip in the frame preceding the return stroke, which is inferred as upward connecting leader considering the physical process of lightning attachment, though not directly confirmed by sequential frames. For stepped leader-first return strokes, the upward connecting leaders tend to be induced by those downward leader branches with brighter luminosity and lower channel tip above ground, and they may accomplish the attachment with great possibility. The upward connecting leaders for 2 out of 61 leader-subsequent stroke sequences were captured in the frame prior to the return stroke, exhibiting relatively long channel lengths of 340 m and 105 m, respectively. The inducing downward subsequent leaders were of the chaotic type characterized by irregular electric field pulse train with duration of 0.2-0.3 ms. The transient drop of the high potential difference between stepped leader system and ground when the attachment occurred would macroscopically terminate the propagation of those ungrounded branches while would not effectively prevent the development of the existing space stem systems in the low-conductivity streamer zone apart from the leader tip. When the ungrounded branches are of poor connection with the main stroke channel, their further propagation toward ground would be feasible. These two factors may contribute to the occurrence of multiple grounding within the same leader-return stroke sequence.
引用
收藏
页码:11,988 / 12,002
页数:15
相关论文
共 41 条
[31]   Strokes of upward illumination occurring within a few milliseconds after typical lightning return strokes [J].
Stolzenburg, Maribeth ;
Marshall, Thomas C. ;
Karunarathne, Sumedhe ;
Karunarathna, Nadeeka ;
Warner, Tom A. ;
Orville, Richard E. ;
Betz, Hans-Dieter .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2012, 117
[32]   LIGHTNING SUBSEQUENT-STROKE ELECTRIC-FIELD PEAK GREATER THAN THE 1ST STROKE PEAK AND MULTIPLE GROUND TERMINATIONS [J].
THOTTAPPILLIL, R ;
RAKOV, VA ;
UMAN, MA ;
BEASLEY, WH ;
MASTER, MJ ;
SHELUKHIN, DV .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D7) :7503-7509
[33]   When does the lightning attachment process actually begin? [J].
Tran, M. D. ;
Rakov, V. A. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2015, 120 (14) :6922-6936
[34]   A negative cloud-to-ground flash showing a number of new and rarely observed features [J].
Tran, M. D. ;
Rakov, V. A. ;
Mallick, S. .
GEOPHYSICAL RESEARCH LETTERS, 2014, 41 (18) :6523-6529
[35]   Observed leader and return-stroke propagation characteristics in the bottom 400 m of a rocket-triggered lightning channel [J].
Wang, D ;
Takagi, N ;
Watanabe, T ;
Rakov, VA ;
Uman, MA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D12) :14369-14376
[36]   Lightning attachment processes of an "anomalous" triggered lightning discharge [J].
Wang, D. ;
Gamerota, W. R. ;
Uman, M. A. ;
Takagi, N. ;
Hill, J. D. ;
Pilkey, J. ;
Ngin, T. ;
Jordan, D. M. ;
Mallick, S. ;
Rakov, V. A. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2014, 119 (03) :1524-1533
[37]   Initiation processes of return strokes in rocket-triggered lightning [J].
Wang, D. ;
Takagi, N. ;
Gamerota, W. R. ;
Uman, M. A. ;
Hill, J. D. ;
Jordan, D. M. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2013, 118 (17) :9880-9888
[38]  
Weidman C.D., 1982, THESIS U ARIZ TUCSON
[39]   LIGHTNING ELECTROMAGNETIC-RADIATION FIELD SPECTRA IN THE INTERVAL FROM 0.2 TO 20 MHZ [J].
WILLETT, JC ;
BAILEY, JC ;
LETEINTURIER, C ;
KRIDER, EP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D12) :20367-20387
[40]   WINTER LIGHTNING ON JAPAN SEA COAST - DEVELOPMENT OF MEASURING SYSTEM ON PROGRESSING FEATURE OF LIGHTNING DISCHARGE [J].
YOKOYAMA, S ;
MIYAKE, K ;
SUZUKI, T ;
KANAO, S .
IEEE TRANSACTIONS ON POWER DELIVERY, 1990, 5 (03) :1418-1425