@Article{CamposSaWaPiKrOr:2014:StAn,
author = "Campos, Leandro Zanella de Souza and Saba, Marcelo Magalh{\~a}es
Fares and Warner, Tom A. and Pinto Jr., Osmar and Krider, E.
Philip and Orville, Richard E.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Department of
Atmospheric Sciences, South Dakota School of Mines and Technology,
Rapid City, SD 57701, USA and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and Institute of Atmospheric Physics, University
of Arizona, Tucson, AZ 85721, USA and Department of Atmospheric
Sciences, Texas A and M University, College Station, TX 77843,
USA",
title = "High-speed video observations of natural cloud-to-ground lightning
leaders - A statistical analysis",
journal = "Atmospheric Research",
year = "2014",
volume = "135-136",
pages = "285–305",
month = "Jan.",
keywords = "lightning, high-speed camera, leaders.",
abstract = "The aim of this investigation is to analyze the phenomenology of
positive and negative (stepped and dart) leaders observed in
natural lightning from digital high-speed video recordings. For
that intent we have used four different high-speed cameras
operating at frame rates ranging from 1000 or 11,800 frames per
second in addition to data from lightning locating systems
(BrasilDat and NLDN). All the recordings were GPS time-stamped in
order to avoid ambiguities in the analysis, allowing us to
estimate the peak current of and the distance to each flash that
was detected by one of the lightning locating systems. The data
collection was done at different sites in south and southeastern
of Brazil, southern Arizona and South Dakota, USA. A total of 62
negative stepped leaders, 76 negative dart leaders and 29 positive
leaders were recorded and analyzed. From these data it was
possible to calculate the two-dimensional speed of each observed
leader, allowing us to obtain its statistical distribution and
evaluate whether or not it is related to other characteristics of
the associated flash. In the analyzed dataset, the speeds of
positive leaders and negative dart leaders follow a lognormal
distribution at the 0.05 level (according to the Shapiro-Wilk
test). We have also analyzed how the two-dimensional leader speeds
change as they approach ground through two different
methodologies. The speed of positive leaders showed a clear
tendency to increase while negative dart leaders tend to become
slower as they approach ground. Negative stepped leaders, on the
other hand, can either accelerate as they get closer to ground or
present an irregular development (with no clear tendency)
throughout their entire development. For all the three leader
types no correlation has been found between the return stroke peak
current and the average speed of the leader responsible for its
initiation. We did find, however, that dart leaders preceded by
longer interstroke intervals cannot present speeds of the order of
107 m s- 1. Finally, we have analyzed the impact of recoil
activity during positive leaders over their average speed and the
return stroke peak current. Even though the analysis considering
the leader speed was not conclusive it was possible to show that
there is no apparent minimum or maximum peak current value for
return strokes preceded by leaders with or without recoil activity
(considering the most common range of values in literature, 20-80
kA). © 2013 Elsevier B.V. All rights reserved.",
doi = "10.1016/j.atmosres.2012.12.011",
url = "http://dx.doi.org/10.1016/j.atmosres.2012.12.011",
issn = "0169-8095",
label = "scopus 2013-11",
language = "en",
targetfile = "1-s2.0-S0169809513000057-main.pdf",
url = "http://dx.doi.org/10.1016/j.atmosres.2012.12.011",
urlaccessdate = "27 abr. 2024"
}