@InProceedings{SchildMeGuHeGoZeNa:2014:AnDeSt,
author = "Schild, Guilherme Touchtenhagen and Meireles, Victor Pezzini and
Gurj{\~a}o, Carlos Diego de Sousa and Held, Gerhard and Gomes,
Ana Maria and Zepka, Gisele dos Santos and Naccarato, Kleber
Pinheiro",
affiliation = "Funda{\c{c}}{\~a}o de Ci{\^e}ncia, Aplica{\c{c}}{\~o}es e
Tecnologias Espaciais (FUNCATE) and Funda{\c{c}}{\~a}o de
Ci{\^e}ncia, Aplica{\c{c}}{\~o}es e Tecnologias Espaciais
(FUNCATE) and Funda{\c{c}}{\~a}o de Ci{\^e}ncia,
Aplica{\c{c}}{\~o}es e Tecnologias Espaciais (FUNCATE) and
{Universidade Estadual Paulista (UNESP)} and {Universidade
Estadual Paulista (UNESP)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "Analysis of the development and structure of a severe storm
leading to the spawning of a tornado in Southeast Brazil",
booktitle = "Proceedings...",
year = "2014",
organization = "International Lightning Detection Conference, 23. (ILDC); and
International Lightning Meteorology Conference, 5 (ILMC).",
keywords = "Tornados, Radar Meteorol{\'o}gico, Descargas Atmosf{\'e}ricas ou
Rel{\^a}mpagos, Tempestades Severas, Previs{\~a}o de Sistemas
Meteorol{\'o}gicos.",
abstract = "During the early afternoon of 22 September 2013, severe storms,
accompanied by large hail, damaging winds, heavy precipitation and
dangerous lightning, devastated a region between 100 and 200 km
south-southwest of the Bauru S-band Doppler radar. Several
extremely intense storm cells moved at up to 100 km/h
east-southeastward and at least one of them spawned a tornado when
it reached the town of Taquarituba, in Southeastern Brazil. The
synoptic pattern was very favorable for the development of severe
weather conditions over southeastern Brazil, due to a cyclogenesis
process that generated an MCS (Mesoscale Convective System), with
a squall line inserted. The convective cells were tracked
throughout their lifetime by IPMetīs Doppler radars. The cells
intensified drastically, with towers overshooting into the
stratosphere (10 dBZ \≤ 20 km) and shortly before reaching
the town of Taquarituba, that particular cell displayed extremely
strong radial shear just above the cloud base, which led to the
formation of a deep meso-cyclone, from which the tornado spawned
and touched down at around 14:30h LT. Before the tornado
touch-down relatively few CG strokes were observed near the
tornadic cell, but thereafter the frequency increased rapidly. The
IC activity was extremely high at most times. WRF model proofed
itself extremely efficient to forecast the severe thunderstorm.",
conference-location = "Tucson",
conference-year = "2014",
label = "lattes: 6324293045209180 7 SchildMeGuHeGoZeNa:2014:AnDeSt",
language = "en",
url = "http://www.vaisala.com/en/events/ildcilmc/Pages/ILDC-2014-archive.aspx",
urlaccessdate = "19 abr. 2024"
}