@InProceedings{LyonsWNCQBLSSRKLBRCZMSSY:2014:MeAsTw,
author = "Lyons, Walter A. and Warner, Tom A. and Nelson, Thomas E. and
Cummins, Kenneth L. and Quick, Mason and Ballweber, Alana and
Lueck, Ryan and Saba, Marcelo Magalh{\~a}es Fares and Schumann,
Carina and Rison, William and Krehbiel, Paul and Lang, Timothy J.
and Beavis, Nicolas and Rutledge, Steven A. and Cummer, Steve A.
and Zigoneanu, Lucian and Myers, Jackson and Samaras, Timothy and
Samaras, Paul and Young, Carl",
affiliation = "FMA Research, Inc., Fort Collins, CO USA and SD School of Mines
and Technology, Rapid City, SD USA and FMA Research, Inc., Fort
Collins, CO USA and {University of Arizona} and {University of
Arizona} and SD School of Mines and Technology, Rapid City, SD USA
and SD School of Mines and Technology, Rapid City, SD USA and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {New Mexico Tech} and
{New Mexico Tech} and NASA MSFC, Huntsville, AL USA and {Colorado
State University} and {Colorado State University} and {Duke
University} and {Duke University} and EDPR, Houston, TX USA and
Samaras Technologies, Bennett, CO USA and Samaras Technologies,
Bennett, CO USA and Samaras Technologies, Bennett, CO USA",
title = "Meteorological Aspects of Two Modes of Lightning-Triggered Upward
Lightning (LTUL) Events in Sprite-Producing MCS",
booktitle = "Proceedings...",
year = "2014",
organization = "International Lightning Detection Conference, 23. (ILDC); and
International Lightning Meteorology Conference, 5 (ILMC).",
keywords = "raio ascendente, sprites, c{\^a}mera de v{\'{\i}}deo de alta
velocidade, campo el{\'e}trico.",
abstract = "Upward lightning from tall objects can be either self-initiated
(SIUL), that is, leaders originating due to locally strong
electric fields but without any preceding lightning, or triggered
by prior lightning discharges in the general vicinity, termed
lightning-triggered upward lightning (LTUL). The LTULs can be
triggered by (1) nearby +CG return strokes propagating through
previous leader networks near the tall object, or (2) the overhead
proximity of horizontally propagating negative stepped leaders
from either IC or +CGs. Examples of both modes of LTULs are
presented. The meteorological environments in which LTULs occur in
the U.S. high plains show a strong similarity to the convective
regimes (trailing MCS stratiform regions) and the parent lightning
which trigger sprites.",
conference-location = "Tucson",
conference-year = "mar. 18-19, 2014 / mar. 20-21, 2014",
label = "lattes: 0505123426174183 8 LyonsWNCQBLSSRKLBRCZMSSY:2014:MeAsTw",
language = "en",
targetfile = "Lyons et al-Meteorological Aspects of Two Modes of
LTUL-2014-ILDC-ILMC.pdf",
urlaccessdate = "03 jun. 2024"
}