@InProceedings{PortugalEcheEchePaci:2018:StStAb,
author = "Portugal, Williamary and Echer, Ezequiel and Echer, Mariza Pereira
de Souza and Pacini, Alessandra Abe",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {National Astronomy and Ionosphere
Center - Arecibo Observatory}",
title = "A statistical study about the effects of Forbush Decrease events
on latitudinal temperature of the near-ground air",
year = "2018",
organization = "Latin American Conference on Space Geophysics, 11. (COLAGE)",
abstract = "We present in this work a statistical study of the near-ground air
temperatures in different latitudes during periods with decrease
of atmospheric ionization induced by Galactic Cosmic Rays (GCR) on
the Earths atmosphere. These GCR fluxes reductions are called
Forbush Decreases (FD), and they are mainly caused by
interplanetary Coronal Mass Ejection (CME) deflection of GCR
around Earth´s orbit. This study was perfomed considering the
possible influence of the cosmogenic atmospheric ionization on the
water vapor condensation patterns (link GCR cloud condensation
nuclei) as the main hypothesis to be tested. For that, we have
conducted a study to analyze these possible effects on the air
surface temperature, using superposed epoch analysis around the
ten strongest FD events occurred between 1987 and 2015. GCR data
were collected from Oulu neutron monitor (cosmicrays.oulu.fi), and
air surface temperature data were obtained from NOAA - National
Oceanic Atmospheric Administration / GSOD - Global Surface Summary
of the Day
(https://data.noaa.gov/dataset/global-surfacesummary-of-the-day-gsod)
of ten meteorological stations of three latitudinal ranges of
Northern and Southern hemispheres (20 - 30, 40 - 50 e 60 - 70). We
investigate here the variation of the daily average of the air
temperature near ground during FD for each one of the three
latitudinal ranges. The possible climatic effects of GCR decrease
were considered using linear and cross correlation methods. The
comparison between the near ground air temperature daily averages
during FD events periods and equivalent periods without FDs
(during solar minima years of 1987, 1996 and 2008) was also
performed. Some results for the Northern hemisphere have showed a
latitudinal dependence of the induced ionization by GCR on the
atmospheric parameters. It was possible to note the anti
correlation between the surface temperature mean and the GCR flux,
increasing from low to high latitudes. However, for the Southern
hemisphere, the anti correlation between these data was only found
for the high and medium latitudes, also with a poleward increase.
From these results it seems that the FD effect on climate is more
prominent in the Northern hemisphere and that there is increases
with latitude.",
conference-location = "Buenos Aires, Argentina",
conference-year = "16-20 abr.",
language = "en",
targetfile = "portugal_statistical.pdf",
urlaccessdate = "28 abr. 2024"
}