@InProceedings{SchuchMBDSLPSBVSHL:2011:SpWeGl,
author = "Schuch, Nelson Jorge and Munakata, Kazuoki and Bieber, John W. and
Duldig, Marcus L. and Sabbah, Ismail and Lago, Alisson Dal and
Petry, Adriano and rigozo, nivaor rodolfo and Silva, Marlos
Rockenbach da and Braga, Carlos Roberto and Vieira, Lucas Ramos
and Stekel, Tardelli Ronan Coelho and souza, mauricio rosa and
Hammerschmitt, Bruno Knevitz and Lima, Roger Hatwig de",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {} and {}
and {} and {} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Space Weather and the Global Muon Detector Network - GMDN",
booktitle = "Proceedings...",
year = "2011",
organization = "12th International Congress of the Brazilian Geophysical Society",
abstract = "The main objective of this work is to present an overview of the
space weather and its relation with the global network of
ground-based multi-directional muon detectors (GMDN). The GMDN is
an international collaboration consisting of 10 institutions from
6 countries in 5 continents. A multi-directional muon detector for
measuring high-energy galactic cosmic rays (GCRs) was installed in
2001 and expanded in its detection area in 2005, through an
international cooperation between Brazil, Japan and USA, and has
been in operation since then at the Southern Space Observatory -
SSO/CRS/INPE -MCT, (29,4º S, 53,8º W, 480 m a.s.l), S{\~a}o
Martinho da Serra, RS, in southern Brazil, as an important
component of the GMDN. The observations conducted by this detector
are used for forecasting the arrival of the interplanetary coronal
mass ejections (ICMEs) and the geomagnetic storms at the Earth.
The detector measures high-energy GCRs by detecting secondary
muons produced from the hadronic interactions of primary GCRs
(mostly protons) with atmospheric nuclei. While muons have a
relatively short life-time (about 2.2 microseconds at rest), they
can reach the detector at ground level because of the relativistic
effect of the time dilation with heir high speed (~0.96c),
preserving the incident direction of primary particles. The
multi-directional detector can measure the GCR intensity in
various directions at a single location, such as SSO in Brazil.
ICMEs accompanied by a strong shock often forms a GCR depleted
region behind the shock. The Forbush decrease is observed when the
Earth enters in this depleted region. Some particles from this
depleted region leak into the downstream, traveling with almost
the speed of light, much faster than the approaching shock, and
creating the precursory loss-cone anisotropy around the sunward
IMF direction at the Earth. Loss-cones are typically visible 4-8
hours prior to the shock arrival and the onset of major
geomagnetic storm at the Earth. This cosmic-ray precursor can be
detected sometimes as early as ten hours prior to the shock
arrival at the Earth. With the real time data from the upgraded
GMDN, its methodology and data reduction techniques permits
accurate Space Weather forecasting.",
conference-location = "Rio de Janeiro",
conference-year = "2011",
label = "lattes: 3638070053255922 7 SchuchMBDSLPSBVSHL:2011:SpWeAn",
language = "en",
targetfile = "Resumo Expandido -Space Weather and-CiSBGF -.pdf",
urlaccessdate = "06 maio 2024"
}