Features of Upward Positive Leaders Initiated From Towers in Natural Cloud‐to‐Ground Lightning Based on Simultaneous High‐Speed Videos, Measured Currents, and Electric Fields

Original simultaneous records of currents, close electric field, and high‐speed videos of natural negative cloud‐to‐ground lightning striking the tower of Morro do Cachimbo Station are used to reveal typical features of upward positive leaders before the attachment, including their initiation and mode of propagation. According to the results, upward positive leaders initiate some hundreds of microseconds prior to the return stroke, while a continuous uprising current of about 4 A and superimposed pulses of a few tens amperes flow along the tower. Upon leader initiation, the electric field measured 50 m away from the tower at ground level is about 60 kV/m. The corresponding average field roughly estimated 0.5 m above the tower top is higher than 0.55 MV/m. As in laboratory experiments, the common propagation mode of upward positive leaders is developing continuously, without steps, from their initiation. Unlike downward negative leaders, upward positive leaders typically do not branch off, though they can bifurcate under the effect of a downward negative leader's secondary branch approaching their lateral surface. The upward positive leader's estimated average two‐dimensional propagation speed, in the range of 0.06 × 106 to 0.16 × 106 m/s, has the same order of magnitude as that of downward negative leaders. Apparently, the speed tends to increase just before attachment.

[1]  S. Visacro,et al.  Unusual features of negative leaders' development in natural lightning, according to simultaneous records of current, electric field, luminosity, and high‐speed video , 2017 .

[2]  Vladislav Mazur,et al.  Principles of Lightning Physics , 2016 .

[3]  Xiushu Qie,et al.  High‐speed video observation of stepwise propagation of a natural upward positive leader , 2016 .

[4]  Martin A. Uman,et al.  Luminosity progression in dart‐stepped leader step formation , 2016 .

[5]  V. Rakov,et al.  High-speed video observations of the fine structure of a natural negative stepped leader at close distance , 2016 .

[6]  Vladimir A. Rakov,et al.  Two basic leader connection scenarios observed in negative lightning attachment process , 2016 .

[7]  Hongbo Zhang,et al.  Burst of intracloud current pulses during the initial continuous current in a rocket‐triggered lightning flash , 2014 .

[8]  Hongbo Zhang,et al.  Characteristics of a rocket‐triggered lightning flash with large stroke number and the associated leader propagation , 2014 .

[9]  Ying Ma,et al.  Three-dimensional propagation characteristics of the upward connecting leaders in six negative tall-object flashes in Guangzhou , 2014 .

[10]  S. Visacro,et al.  Assessing currents of upward lightning measured in tropical regions , 2014 .

[11]  M. D. Tran,et al.  A negative cloud‐to‐ground flash showing a number of new and rarely observed features , 2014 .

[12]  William H. Beasley,et al.  High‐speed video observations of a natural negative stepped leader and subsequent dart‐stepped leader , 2013 .

[13]  Xiushu Qie,et al.  Propagating features of upward positive leaders in the initial stage of rocket-triggered lightning , 2013 .

[14]  F. Heidler,et al.  The Slow-Varying Electric Field of Negative Upward Lightning Initiated by the Peissenberg Tower, Germany , 2013, IEEE Transactions on Electromagnetic Compatibility.

[15]  Richard E. Orville,et al.  High-speed video and electric field observation of a negative upward leader connecting a downward positive leader in a positive cloud-to-ground flash , 2013 .

[16]  Silverio Visacro,et al.  Updated statistics of lightning currents measured at Morro do Cachimbo Station , 2012 .

[17]  Tom A. Warner,et al.  Observations of simultaneous upward lightning leaders from multiple tall structures , 2012 .

[18]  Kenneth L. Cummins,et al.  Upward lightning observations from towers in Rapid City, South Dakota and comparison with National Lightning Detection Network data, 2004-2010 , 2012 .

[19]  M. Uman,et al.  Observations of the initial, upward‐propagating, positive leader steps in a rocket‐and‐wire triggered lightning discharge , 2011 .

[20]  Martin A. Uman,et al.  High-speed video observations of a lightning stepped leader , 2011 .

[21]  Daohong Wang,et al.  A downward positive leader that radiated optical pulses like a negative stepped leader , 2011 .

[22]  Vladimir A. Rakov,et al.  Observations of stepping mechanisms in a rocket‐and‐wire triggered lightning flash , 2010 .

[23]  S. Visacro,et al.  Early phase of lightning currents measured in a short tower associated with direct and nearby lightning strikes , 2010 .

[24]  X. Qie,et al.  Characteristics of downward leader in a positive cloud‐to‐ground lightning flash observed by high‐speed video camera and electric field changes , 2008 .

[25]  J. Jerauld,et al.  Experimental Study of Lightning-Induced Currents in a Buried Loop Conductor and a Grounded Vertical Conductor , 2008, IEEE Transactions on Electromagnetic Compatibility.

[26]  Marco Aurélio O. Schroeder,et al.  Statistical analysis of lightning current parameters: Measurements at Morro do Cachimbo Station , 2004 .

[27]  Taku Noda,et al.  Charge-Voltage curves of surge corona on transmission lines: two measurement methods , 2003 .

[28]  Eduard M. Bazelyan,et al.  Lightning Physics and Lightning Protection , 2000 .

[29]  S. Yokoyama,et al.  Winter lightning on Japan Sea coast-development of measuring system on progressing feature of lightning discharge , 1990 .

[30]  I. Gallimberti,et al.  The mechanism of the long spark formation , 1979 .

[31]  H. Singer,et al.  A Charge Simulation Method for the Calculation of High Voltage Fields , 1974 .

[32]  K. Berger,et al.  Novel observations on lightning discharges: Results of research on Mount San Salvatore , 1967 .