RF and X-ray source locations during the lightning attachment process

被引:48
作者
Howard, J. [1 ]
Uman, M. A. [1 ]
Biagi, C. [1 ]
Hill, D. [1 ]
Jerauld, J. [1 ]
Rakov, V. A. [1 ]
Dwyer, J. [2 ]
Saleh, Z. [2 ]
Rassoul, H. [2 ]
机构
[1] Univ Florida, Dept Elect & Comp Engn, Gainesville, FL 32611 USA
[2] Florida Inst Technol, Dept Phys & Space Sci, Melbourne, FL 32901 USA
基金
美国国家科学基金会;
关键词
RADIATION-FIELDS; FINE-STRUCTURE; BREAKDOWN; SYSTEM; CURRENTS; DE/DT;
D O I
10.1029/2009JD012055
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Using an eight-station array of electric field derivative (dE/dt) sensors and colocated NaI X-ray detectors, we have obtained 3-D RF source locations during the leaders and attachment processes of three first strokes initiated by stepped leaders in natural cloud-to-ground lightning and one stroke initiated by a dart-stepped leader in a rocket-and-wire triggered flash. Stepped leader and dart-stepped leader dE/dt pulses are tracked from a few hundred meters to a few tens of meters above ground, after which pulses of different characteristics than the step pulses are observed to occur at lower altitudes. These postleader pulses include: (1) the "leader burst,'' a group of pulses in the dE/dt waveform occurring just prior to the slow front in the corresponding return-stroke electric field waveform; (2) dE/dt pulses occurring during the slow front; and (3) the fast-transition or dominant dE/dt pulse that is usually associated with the rapid transition to peak in the return-stroke electric field waveform. Additionally, the timing coincidence between X rays and dE/dt pulses on colocated measurements is used to examine the X-ray production by the postleader processes. Leader bursts (LBs) are the largest X-ray producers of the three postleader processes and exhibit propagation speeds that exceed the preceding stepped leader speeds by more than an order of magnitude. Slow-front (SF) and fast-transition pulses appear to originate from similar physical processes, probably the multiple connections of upward and downward leaders. However, more X-rays are coincident with slow-front pulses than with fast-transition pulses.
引用
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页数:25
相关论文
共 51 条
[41]   Accuracy of the Lightning Mapping Array [J].
Thomas, RJ ;
Krehbiel, PR ;
Rison, W ;
Hunyady, SJ ;
Winn, WP ;
Hamlin, T ;
Harlin, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D14) :D14207
[42]   SYSTEM FOR LOCATING THE SOURCES OF WIDE-BAND DE/DT FROM LIGHTNING [J].
THOMSON, EM ;
MEDELIUS, PJ ;
DAVIS, S .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D11) :22793-22802
[43]   CURRENTS IN FLORIDA LIGHTNING RETURN STROKES [J].
UMAN, MA ;
MCLAIN, DK ;
FISHER, RJ ;
KRIDER, EP .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (18) :3530-3537
[44]   Statistical analysis of lightning current parameters: Measurements at Morro do Cachimbo Station [J].
Visacro, S ;
Soares, A ;
Schroeder, MAO ;
Cherchiglia, LCL ;
de Sousa, VJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D1)
[45]   Attachment process in rocket-triggered lightning strokes [J].
Wang, D ;
Rakov, VA ;
Uman, MA ;
Takagi, N ;
Watanabe, T ;
Crawford, DE ;
Rambo, KJ ;
Schnetzer, GH ;
Fisher, RJ ;
Kawasaki, ZI .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D2) :2143-2150
[46]  
WANG DM, 2001, 2001 INT AER GROUND
[47]   FINE-STRUCTURE OF LIGHTNING RETURN STROKE WAVE FORMS [J].
WEIDMAN, CD ;
KRIDER, EP .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1978, 83 (NC12) :6239-6247
[48]  
WEIDMAN CD, 1986, 1986 INT AER GROUND
[49]   SUBMICROSECOND INTERCOMPARISON OF RADIATION-FIELDS AND CURRENTS IN TRIGGERED LIGHTNING RETURN STROKES BASED ON THE TRANSMISSION-LINE MODEL [J].
WILLETT, JC ;
BAILEY, JC ;
IDONE, VP ;
EYBERTBERARD, A ;
BARRET, L .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D11) :13275-13286
[50]   AN EXPERIMENTAL TEST OF THE TRANSMISSION-LINE MODEL OF ELECTROMAGNETIC-RADIATION FROM TRIGGERED LIGHTNING RETURN STROKES [J].
WILLETT, JC ;
IDONE, VP ;
ORVILLE, RE ;
LETEINTURIER, C ;
EYBERTBERARD, A ;
BARRET, L ;
KRIDER, EP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1988, 93 (D4) :3867-3878