@InProceedings{NunesCoelKuboHegg:2020:DyRaEf,
author = "Nunes, Mateus Dias and Coelho, Simone Marilene Sievert da Costa
and Kubota, Paulo Yoshio and Hegglin, Michaela I.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {University of Reading}",
title = "Dynamic and radiative effects of stratospheric ozone on
atmospheric blocking in Southern South America",
booktitle = "Resumos.../P{\^o}steres",
year = "2020",
editor = "Galetti, Giovana Deponte and Sena, Caio {\'A}tila Pereira and
Mand{\'u}, Tiago Bentes and Jacondino, William Duarte and Alves,
Laurizio Emanuel Ribeiro and Afonso, Eliseu Oliveira Afonso",
organization = "Encontro dos Alunos de P{\'o}s-Gradua{\c{c}}{\~a}o em
Meteorologia do CPTEC/INPE, 19. (EPGMET)",
publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
address = "S{\~a}o Jos{\'e} dos Campos",
keywords = "Total Ozone Column, Stratosphere-Troposphere, Potential
Vorticity.",
abstract = "The present research aimed to identify the patterns associated
with exchanges in the Upper Troposphere and Lower Stratosphere and
the relationship between stratospheric ozone and atmospheric
blocking. Eighteen cases of atmospheric blocks that occurred in
the region between the Southeast Pacific and the South Atlantic in
the period between 2000-2015 for the winter months of
June-July-August (JJA) were selected. To describe the processes
that occur in the stratosphere-troposphere coupling, mass flux,
and rates of radiative heating and cooling at high levels of the
atmosphere were evaluated. It was observed that the intrusion of a
stratospheric is characterized by potential anomalies of vorticity
and a high concentration of stratospheric ozone in the atmospheric
column. Through the analysis of the dynamic tropopause and based
on the ozone content within an atmospheric column, the anomalies
of potential vorticity coincided with regions with the largest
amounts of the ozone column and downward flux, favoring the
intrusion of stratospheric ozone into the upper troposphere
region. In the region of the atmospheric block, positive
temperature anomalies higher levels are observed and are
associated with rates of radiative heating/cooling due to
variations in ozone in the stratosphere. Besides, the vorticity
anomalies between 1.5 and 2 PVU contributed to the decrease of the
geopotential height in the tropospheric column that favors the
formation of the atmospheric blocking.",
conference-location = "Online",
conference-year = "16-19 nov. 2020",
language = "pt",
organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
ibi = "8JMKD3MGPDW34R/43MD9SE",
url = "http://urlib.net/ibi/8JMKD3MGPDW34R/43MD9SE",
targetfile = "GT1_NUNESMATEUSDIAS_XIX_EPGMET.docx - Mateus Dias Nunes.pdf",
type = "Estudos e Modelagem do Tempo e Clima",
urlaccessdate = "09 maio 2024"
}