Initial results of LF sensor network for lightning observation and characteristics of lightning emission in LF band

We have been developing an LF sensor network called Broadband Observation network for Lightning and Thunderstorm (BOLT), to image the structure of lightning discharges in 3D using time of arrival (TOA) technique. This paper documents initial results and characteristics of BOLT source locations for further understanding of LF radiation associated with lightning. Theoretical reduced Chi-square distribution fitted to BOLT observation data indicates a root mean square (rms) timing error of about 200 ns for each sensor. Monte Carlo simulations of BOLT indicate that at an altitude of 5000 m the standard deviations for horizontal differences between a known source and a location that the BOLT algorithm produces are less than 200 m, and vertical differences are less than 400 m in most of the network. Furthermore, comparison of BOLT and VHF source locations arriving at the same site within 5 µs indicates that the average difference for elevation direction is 0.73° with a standard deviation of 3.64°, and that for the azimuth direction is 0.58° with a standard deviation of 1.98°. Lightning flash processes of intracloud (IC) and cloud-to-ground (CG) flashes, including preliminary breakdown pulses, negative leaders, breakdown in the negative charge region (NCR), and an attempted leader, are well imaged by BOLT. Normalized amplitudes in E-field change waveform of BOLT sources associated with negative leaders and breakdown occurred in the NCR do not have significant difference, implying that most BOLT sources in the NCR might be associated with negative recoil leaders.

[1]  Akimasa Hirata,et al.  An Operational VHF Broadband Digital Interferometer for Lightning Monitoring , 2004 .

[2]  Michael Stock,et al.  Total Lightning Observations with the New and Improved Los Alamos Sferic Array (LASA) , 2006 .

[3]  Tomoo Ushio,et al.  An Error Estimate of the VHF Broadband Digital Interferometer , 2009 .

[4]  Xuan-Min Shao,et al.  Radio interferometric observations of cloud‐to‐ground lightning phenomena in Florida , 1995 .

[5]  K. Schmidt,et al.  Lightning detection with 3‐D discrimination of intracloud and cloud‐to‐ground discharges , 2004 .

[6]  Martin A. Uman,et al.  Co‐location of lightning leader x‐ray and electric field change sources , 2008 .

[7]  David M. Suszcynsky,et al.  Relationships among Narrow Bipolar Events, “total” lightning, and radar‐inferred convective strength in Great Plains thunderstorms , 2008 .

[8]  Vladimir A. Rakov,et al.  Three‐dimensional imaging of upward positive leaders in triggered lightning using VHF broadband digital interferometers , 2010 .

[9]  Steven J. Goodman,et al.  North Alabama Lightning Mapping Array (LMA): VHF Source Retrieval Algorithm and Error Analyses , 2004 .

[10]  K. Schmidt,et al.  LINET—An international lightning detection network in Europe , 2009 .

[11]  Tomoo Ushio,et al.  Broadband and narrowband RF interferometers for lightning observations , 2000 .

[12]  M. Stock,et al.  Continuous broadband digital interferometry of lightning using a generalized cross‐correlation algorithm , 2014 .

[13]  S. E. Reynolds,et al.  THUNDERSTORM CHARGE SEPARATION , 1957 .

[14]  Hitoshi Sakurano,et al.  Upward Lightning Observed by LF Broadband Interferometer , 2013 .

[15]  Hartmut Höller,et al.  Cloud Lightning: Detection and Utilization for Total Lightning Measured in the VLF/LF Regime , 2007 .

[16]  Ting Wu,et al.  Comparison of positive and negative compact intracloud discharges , 2011 .

[17]  J. Montanyà,et al.  Asymmetries in bidirectional leader development of lightning flashes , 2013 .

[18]  Richard E. Orville,et al.  Lightning leader characteristics in the Thunderstorm Research International Program (TRIP) , 1982 .

[19]  Tomoo Ushio,et al.  What occurs in K process of cloud flashes , 2010 .

[20]  Abram R. Jacobson,et al.  Comparison of Narrow Bipolar Events with Ordinary Lightning as Proxies for Severe Convection , 2005 .

[21]  X. Shao,et al.  RF radiation observations of positive cloud‐to‐ground flashes , 1999 .

[22]  Vernon Cooray,et al.  Comparative study on preliminary breakdown pulse trains observed in Johor, Malaysia and Florida, USA , 2012 .

[23]  Vladimir A. Rakov,et al.  Some inferences on the role of lower positive charge region in facilitating different types of lightning , 2009 .

[24]  Tsutomu Takahashi,et al.  Riming Electrification as a Charge Generation Mechanism in Thunderstorms , 1978 .

[25]  Z. Kawasaki,et al.  Verification of Bi-directional Leader Concept by Interferometer Observations , 2002 .

[26]  Tomoo Ushio,et al.  Propagation characteristics of lightning stepped leaders developing in charge regions and descending out of charge regions , 2012 .

[27]  Eric C. Bruning,et al.  Lightning Activity in a Hail-Producing Storm Observed with Phased-Array Radar , 2011 .

[28]  Harald E. Edens,et al.  VHF lightning mapping observations of a triggered lightning flash , 2012 .

[29]  V. Mazur,et al.  Model of electric charges in thunderstorms and associated lightning , 1998 .

[30]  Abram R. Jacobson,et al.  A method for determining intracloud lightning and ionospheric heights from VLF/LF electric field records , 2004 .

[31]  Ting Wu,et al.  Spatial relationship between lightning narrow bipolar events and parent thunderstorms as revealed by phased array radar , 2013 .

[32]  Tomoo Ushio,et al.  Effects of Charge Distribution in Thunderstorms on Lightning Propagation Paths in Darwin, Australia , 2011 .

[33]  Dong Zheng,et al.  Observation of compact intracloud discharges using VHF broadband interferometers: CHARACTERISTICS OF CID CHANNELS , 2012 .

[34]  D. Marquardt An Algorithm for Least-Squares Estimation of Nonlinear Parameters , 1963 .

[35]  D. M. Suszcynsky,et al.  Narrow Bipolar Events as indicators of thunderstorm convective strength , 2003 .

[36]  Z. Kawasaki,et al.  Leader process in 3D observed by VLF/LF broadband interferometer , 2012, 2012 International Conference on Lightning Protection (ICLP).

[37]  E. Williams Problems in lightning physics—the role of polarity asymmetry , 2006 .

[38]  P. Krehbiel,et al.  Accuracy of the Lightning Mapping Array , 2003 .

[39]  Ken-ichi Shimose,et al.  Three-Dimensional VHF Lightning Mapping System for Winter Thunderstorms , 2013 .

[40]  O. Pinto,et al.  Cloud‐to‐ground lightning flash characteristics in southeastern Brazil for the 1992–1993 summer season , 1996 .

[41]  N. Kitagawa,et al.  A comparison of intracloud and cloud-to-ground lightning discharges , 1960 .

[42]  E. Philip Krider,et al.  The radiation field wave forms produced by intracloud lightning discharge processes , 1979 .

[43]  Thomas C. Marshall,et al.  Locating initial breakdown pulses using electric field change network , 2013 .

[44]  Ting Wu,et al.  Large bipolar lightning discharge events in winter thunderstorms in Japan , 2014 .

[45]  S. Cummer,et al.  Initial breakdown pulses in intracloud lightning flashes and their relation to terrestrial gamma ray flashes , 2013 .

[46]  Masahito Shimizu,et al.  Preliminary breakdown pulses of cloud-to-ground lightning in winter thunderstorms in Japan , 2013 .

[47]  Ting Wu,et al.  Lightning Observation in 3D using a Multi LF Sensor Network and Comparison with Radar Reflectivity , 2014 .

[48]  John M. Hall,et al.  Characterization and applications of VLF/LF source locations from lightning using the Huntsville Alabama Marx Meter Array , 2013 .

[49]  Vladimir A. Rakov,et al.  On phenomenology of compact intracloud lightning discharges , 2010 .

[50]  Vladimir A. Rakov,et al.  The initial stage processes of rocket‐and‐wire triggered lightning as observed by VHF interferometry , 2012 .

[51]  Manabu Akita,et al.  Data processing procedure using distribution of slopes of phase differences for broadband VHF interferometer , 2014 .

[52]  Paul Krehbiel,et al.  Observations of VHF source powers radiated by lightning , 2001 .

[53]  Vladimir A. Rakov,et al.  Pulse trains that are characteristic of preliminary breakdown in cloud‐to‐ground lightning but are not followed by return stroke pulses , 2008 .

[54]  Y. Honda,et al.  A pre‐operational variational data assimilation system for a non‐hydrostatic model at the Japan Meteorological Agency: formulation and preliminary results , 2005 .