@InProceedings{JaskulskiScAvMoMoDeMu:2007:StSoAt,
author = "Jaskulski, Tiago and Schuch, Nelson Jorge and Aveiro, Henrique
Carlotto and Moor, Lilian Piecha and Moro, Juliano and Denardini,
Clezio Marcos and Muralikrishna, Polinaya",
affiliation = "Southern Space Observatory, National Institute for Space Research,
Santa Maria - RS), Brazil and Southern Space Observatory, National
Institute for Space Research, Santa Maria - RS), Brazil and
Southern Space Observatory, National Institute for Space Research,
Santa Maria - RS), Brazil and Southern Space Observatory, National
Institute for Space Research, Santa Maria - RS), Brazil and Space
Science Laboratory of Santa Maria - LACESM/CT - UFSM, Santa Maria,
RS, Brazil and {National Institute for Space Research –
DAE/CEA/INPE – MCT} and {National Institute for Space Research –
DAE/CEA/INPE – MCT}",
title = "Study of the South Atlantic Magnetic Anomaly Influence on the
Energetic Particle Precipitation",
booktitle = "Proceedings...",
year = "2007",
organization = "IUGG General Assembly, 24.",
keywords = "Geomagnetic-anomaly, particle-precipitation, imaging-riometer –
Aeronomia.",
abstract = "The South Atlantic Magnetic Anomaly (SAMA), localized in the South
Hemisphere, reaches almost all the region of the South Atlantic
and extends longitudinally until the west coast of the South
America. It is characterized as a region where the geomagnetic
field has its lowest intensity and, therefore, there is a
depression in its Field lines intensity. This depression anomaly
occurs only in this region of the planet and its origin is
attributed to the anti-symmetrical distribution of the electric
currents in the interior of the planet. One of the consequences of
the low intensity of the geomagnetic field in this region is that
the energetic particles trapped in the Van Allens inner radiation
belt can precipitate easily. The mirror point of the trapped
particles over the SAMA is approximately 100 km of altitude, while
is around 600 km in the magnetic conjugate point in the north
hemisphere. In virtue of this, these energetic particles can
precipitate over this region and dissipate their energy ionizing
the atmospheric components, as occurs in the auroral region. This
process is further enhanced during periods of geomagnetic storms
and substorms. One of the usual methods to study the particle
precipitation in the SAMA is through of the Imaging Riometer. The
level of ionospheric absorption of cosmic noise is indirectly
obtained from the data acquired with this equipment. From this
data it is possible to infer the variation of the ionosphere
electronic density. A higher ionospheric absorption indicates that
an increase in the electronic density could have occurred in
consequence of the energetic particle precipitation. Currently,
there are three Imaging Riometer equipments in the SAMA region.
The first one was installed in 1999 in the Southern Space
Observatory - SSO/CRS/INPE - MCT, in S{\~a}o Martinho da Serra,
Brazil, (29.4ºS, 53.8ºW). This observatory is strategically
located near of the SAMA center, where the intensity of
geomagnetic field is around of 23000 nT. In 2003 the second
equipment was installed in Punta Arenas, Chile (53.1ºS, 71.0ºW).
The third one was installed in Concepcion, Chile (37.5ºS, 72.7ºW).
From these three equipments it has been possible to carry out
studies to determine spatial scale and movement of the events of
ionospheric absorption. The objective of this work is to present
the analysis of data observed during a magnetically disturbed
period with the Imaging Riometer installed at the Southern Space
Observatory, as well as to give its brief description.",
conference-location = "Perugia, Italy",
conference-year = "2-13 July",
language = "en",
urlaccessdate = "16 jun. 2024"
}