Model of sprite luminous trail caused by increasing streamer current

[1] This study investigates a possible physical mechanism responsible for the occurrence of the luminous trail of sprite streamers, which is also known as “afterglow.” According to streamer modeling results, when sprite streamers propagate with expansion, acceleration and brightening, the total current flowing through the streamer body also increases. The increasing current results in the rise of the electric field in the streamer channel far behind the streamer head, which leads to effective production of N2 excited states by electron impact excitation and then the glowing trail.

[1]  S. Cummer,et al.  Testing sprite initiation theory using lightning measurements and modeled electromagnetic fields , 2007 .

[2]  Ningyu Liu,et al.  Molecular nitrogen LBH band system far‐UV emissions of sprite streamers , 2005 .

[3]  M. McHarg,et al.  Comparison of acceleration, expansion, and brightness of sprite streamers obtained from modeling and high-speed video observations , 2008 .

[4]  T. E. Nelson,et al.  Submillisecond imaging of sprite development and structure , 2006 .

[5]  Matthew G. McHarg,et al.  Altitude resolved sprite spectra with 3 ms temporal resolution , 2007 .

[6]  Matthew G. McHarg,et al.  Plasma chemistry of sprite streamers , 2007 .

[7]  D. Sentman,et al.  Chemical effects of weak electric fields in the trailing columns of sprite streamers , 2009 .

[8]  Matthew J. Heavner,et al.  N 2( B 3 ? g) and N 2 +( A 2 ? u) vibrational distributions observed in sprites , 2003 .

[9]  S. Cummer,et al.  Measurement of sprite streamer acceleration and deceleration , 2009 .

[10]  W. Shockley Currents to Conductors Induced by a Moving Point Charge , 1938 .

[11]  Matthew G. McHarg,et al.  Observed emission rates in sprite streamer heads , 2007 .

[12]  Lou‐Chuang Lee,et al.  Assessment of sprite initiating electric fields and quenching altitude of a1Πg state of N2 using sprite streamer modeling and ISUAL spectrophotometric measurements , 2009 .

[13]  Umran S. Inan,et al.  Sprites produced by quasi‐electrostatic heating and ionization in the lower ionosphere , 1997 .

[14]  F. J. Gordillo-Vazquez,et al.  Air plasma kinetics under the influence of sprites , 2008 .

[15]  T. Bell,et al.  Spatial structure of sprites , 1998 .

[16]  S. Ramo Currents Induced by Electron Motion , 1939, Proceedings of the IRE.

[17]  Ningyu Liu,et al.  Effects of photoionization on propagation and branching of positive and negative streamers in sprites , 2004 .

[18]  Matthew G. McHarg,et al.  Observations of streamer formation in sprites , 2007 .

[19]  Remo Guidieri Res , 1995, RES: Anthropology and Aesthetics.

[20]  C. Jen,et al.  On the Induced Current and Energy Balance in Electronics , 1941, Proceedings of the IRE.

[21]  F J Gordillo-V Air plasma kinetics under the influence of sprites , 2008 .

[22]  Ute Ebert,et al.  Emergence of sprite streamers from screening-ionization waves in the lower ionosphere , 2009 .

[23]  Eugene M. Wescott,et al.  Time resolved N2 triplet state vibrational populations and emissions associated with red sprites , 1998 .

[24]  Mikhail N. Shneider,et al.  Long streamers in the upper atmosphere above thundercloud , 1998 .

[25]  V. Pasko Red sprite discharges in the atmosphere at high altitude: the molecular physics and the similarity with laboratory discharges , 2007 .

[26]  Matthew G. McHarg,et al.  High time-resolution sprite imaging: observations and implications , 2008 .