@Article{SaraivaCWZAPHBBMB:2014:HiViEl,
author = "Saraiva, Antonio Carlos Varela and Campos, Leandro Zanella de
Souza and Williams, E. R. and Zepka, Gisele dos Santos and Alves,
J. and Pinto Junior, Osmar and Heckman, S. and Buzato, Tiago
Santos and Bailey, J. C. and Morales, C. A. and Blakeslee, R. J.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Massachusetts
Institute of Technology} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Earth Networks} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {University of Alabama in Huntsville} and
{Universidade de S{\~a}o Paulo (USP. IAG)} and {NASA Marshall
Space Flight Center}",
title = "High-speed video and electromagnetic analysis of two natural
bipolar cloud-to-ground lightning flashes",
journal = "Journal of Geophysical Research D",
year = "2014",
volume = "119",
number = "10",
pages = "6105--6127",
abstract = "High-speed video records of two bipolar cloud-to-ground flashes
were analyzed in detail. They both began with a single positive
return stroke that was followed by more than one subsequent weak
negative stroke. Due to the elevated cloud base height of its
parent thunderstorm, the preparatory processes of each subsequent
negative stroke were documented optically below cloud base. In the
first event (Case 1) it was observed that all four subsequent
negative strokes were initiated by recoil leaders that retraced
one horizontal channel segment previously ionized by the positive
leader. Those recoil leaders connected to the original vertical
channel segment and propagated toward ground, producing four
subsequent strokes that had the same ground contact point as the
original positive discharge. The second event (Case 2), in
contrast, presented 15 subsequent strokes that were initiated by
recoil leaders that did not reach the original channel of the
positive stroke. They diverged vertically toward ground, making
contact approximately 11 km away from the original positive strike
point. These results constitute the first optical evidence that
both single- and multiple-channel bipolar flashes occur as a
consequence of recoil leader activity in the branches of the
initial positive return stroke. For both events their total
channel length increased continuously at a rate of the order of
104 m s-1, comparable to speeds reported for typical positive
leaders. Key Points Inception of subsequent strokes of natural
bipolar cloud-to-ground flashes First report of inception
mechanism of negative phase of bipolar CG flashes High-speed
camera and multiple LLS study of bipolar CG flashes ©2014.
American Geophysical Union. All Rights Reserved.",
doi = "10.1002/2013JD020974",
url = "http://dx.doi.org/10.1002/2013JD020974",
issn = "0148-0227",
label = "scopus 2014-07 SaraivaCWZAPHBBMB:2014:HiViEl",
language = "en",
urlaccessdate = "27 abr. 2024"
}