@InProceedings{PereiraSoaLemPinSch:2009:SeEfAn,
author = "Pereira, Nadiara and Soares, Ana Marceli and Leme, Neusa Paes and
Pinheiro, Damaris Kirsh and Schuch, Nelson Jorge",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {} and {} and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Secondary effects of antarctic ozone hole in Southern Brazil for
the year 2008, a case study",
year = "2009",
organization = "IACS Joint Assembly.",
abstract = "The Antarctic continent shows a significant decrease of the total
ozone content during the austral spring, from where air mass with
poor ozone content can move generating secondary effects of the
Antarctic Ozone Hole in low latitudes. The total ozone column data
from Brewer Spectrophotometer is monitored at the Southern Space
Observatory - OES/CRS/CIE/INPE - MCT (29.42° S, 53.87°W), S{\~a}o
Martinho da Serra, Brazil, in a cooperation between Space Science
Laboratory of Santa Maria LACESM/CT/UFSM, Southern Regional Center
for Space Science CRS/CIE/INPE MCT and Ozone Laboratory
LO/DGE/CEA/INPE MCT. Ozone data from OMI on board NASA Satellite
and data from NCEP reanalysis are also used in this analysis. The
methodology is based in the analysis of potential vorticity on
isentropic surfaces for days with low ozone total column from
Brewer and OMI for 2008. Potential vorticity, which behaves as a
dynamical tracer in the absence of diabatic effects, can be used
to study the transport of air masses on isentropic surfaces in the
stratosphere. The year of 2008 showed one event with decreased in
the ozone measures in the Southern Space Observatory linked with
the Antarctic Region, October 21th. The obtained results show the
influence of air masses with poor ozone content on the central
region of the Rio Grande do Sul state in Southern Brazil with a
decrease to 271.5 DU, when the climatology for the region in the
months of October is 292.9 ± 9.5 DU. The isentropic air mass back
trajectories also proved the polar origin of the air masses.",
conference-location = "Montreal, Canada",
conference-year = "July, 19-29",
language = "en",
targetfile = "Abstract IAMAS 2009_NADIARA-1.pdf",
urlaccessdate = "12 maio 2024"
}