@Article{BragaLagKuwSchMun:2013:TeEfCo,
author = "Braga, Carlos Roberto and Lago, Alisson Dal and Kuwabara, T and
Schuch, Nelson Jorge and Munakata, K",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Bartol Research
Institute, University of Delaware, Newark (DE), USA and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Physics Department,
Faculty of Science, Shinshu University, Matsumoto, Japan",
title = "Temperature effect correction for the cosmic ray muon data
observed at the Brazilian Southern Space Observatory in S{\~a}o
Martinho da Serra",
journal = "Journal of Physics: Conference Series",
year = "2013",
volume = "409",
pages = "012138",
note = "23rd European Cosmic Ray Symposium (ECRS) / 32nd Russian Cosmic
Ray Conference, Lomonosov Moscow State Univ, Moscow, RUSSIA, July
03-07, 2012",
keywords = "temperature, cosmic ray, muon, Brazil, atmospheric expansion.",
abstract = "The negative atmospheric temperature effect observed in the muon
intensity measured by surface-level detectors is related to the
atmospheric expansion during summer periods. According the first
explanation given, the path of muons from the higher atmospheric
level (where they are generated) to the ground becomes longer, and
more muons decay, leading to a muon intensity decrease. A
significant negative correlation, therefore, is expected between
the altitude of the equi-pressure surface and the muon intensity.
We compared measurements of the altitude of 100 hPa equi-pressure
surface and data from the multidirectional muon detector installed
at the Brazilian Southern Space Observatory in S{\~a}o Martinho
da Serra, RS. Significant correlation coefficient were found (up
to 0.95) when using data observed in 2008. For comparison, data
from the multidirectional muon detector of Nagoya, located in the
opposite hemisphere, is studied and an anti-phase in the cosmic
ray variation related with the temperature effect is expected
between data from detectors of Nagoya and S{\~a}o Martinho da
Serra. The temperature influence is higher for the directional
channels of Nagoya than for ones of S{\~a}o Martinho da Serra.",
doi = "10.1088/1742-6596/409/1/012138",
url = "http://dx.doi.org/10.1088/1742-6596/409/1/012138",
issn = "1742-6588",
label = "lattes: 2768849231719678 2 BragaLagKuwSchMun:2013:TeEfCo",
language = "en",
targetfile = "1742-6596_409_1_012138.pdf",
urlaccessdate = "02 maio 2024"
}