@Article{CruzSabaSchuWarn:2022:UpBiLi,
author = "Cruz, Ivan Toucedo and Saba, Marcelo Magalh{\~a}es Fares and
Schumann, Carina and Warner, Tom A.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {University of the
Witwatersrand} and {ZT Research}",
title = "Upward Bipolar Lightning Flashes Originated From the Connection of
Recoil Leaders With Intracloud Lightning",
journal = "Geophysical Research Letters",
year = "2022",
volume = "49",
number = "22",
pages = "1",
keywords = "The present work shows high-speed videos of two upward flashes
that started with positive upward leaders and, instead of being
followed by negative subsequent return strokes, they were followed
by positive subsequent return strokes. In both cases, after the
positive leaders developed, recoil leaders (RL) appeared in their
decayed branches as would be usual in negative upward lightning
flashes. However, in these flashes the negative end of a recoil
leader connected to a positive leader of an intracloud (IC) flash
nearby. The connection initiated a downward positive leader that
re-ionized the decayed channel of the upward flash all the way to
the tower giving origin to a positive subsequent return stroke.
This work shows that RL do play an important role in the
occurrence of bipolar upward flashes and their interaction with IC
flashes can provide explanations for all types of bipolar upward
flashes initiated by upward positive leaders.Plain Language
SummaryThe increasing number of tall buildings and towers, and the
rapid expansion of wind power generation, has also increased the
concerns about damages caused by upward flashes. Although upward
flashes are not the most common type of flashes in nature, they
can pose a serious threat to tall structures. They are usually
initiated by a positive upward leader that starts at the tip of
the structure. After reaching cloud base, the discharge ends or is
followed by a negative downward leader that strikes the tower and
produces an intense negative discharge known as a return stroke.
This common type of upward flash is named negative upward flash.
The present work presents high-speed videos of a rare type of
upward flash, the bipolar upward flash. In this flash, after the
propagation of the positive upward leader, another positive leader
retraces the same path traveled by the original upward leader, but
in a downward manner resulting in a positive return stroke. The
increased threat of damage caused by this rare flash is due to the
intense positive return stroke and long duration current that
frequently follows. This work explains how this, and other types
of bipolar flashes are possible.",
doi = "10.1029/2022GL101072",
url = "http://dx.doi.org/10.1029/2022GL101072",
issn = "0094-8276",
label = "lattes: 2485050167650687 1 CruzSabaSchuWarn:2022:UpBiLi",
language = "en",
targetfile = "Geophysical Research Letters - 2022 - Cruz - Upward Bipolar
Lightning Flashes Originated From the Connection of Recoil.pdf",
urlaccessdate = "16 jun. 2024"
}