@Article{PaulinoPCABTWSMB:2020:SeOsOb,
author = "Paulino, Igo and Paulino, Ana Roberta and Cueva, Ricardo Y. C. and
Agyei-Yeboah, Ebenezer and Buriti, Ricardo Arlen and Takahashi,
Hisao and Wrasse, Cristiano Max and Santos, {\^A}ngela Machado
dos and Medeiros, Amauri Fragoso de and Batista, Inez Staciarini",
affiliation = "{Universidade Federal de Campina Grande (UFCG)} and {Universidade
Federal da Para{\'{\i}}ba (UFPB)} and {Universidade Federal do
Maranh{\~a}o (UFMA)} and {Universidade do Vale do
Para{\'{\i}}ba (UNIVAP)} and {Universidade Federal de Campina
Grande (UFCG)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade Federal de Campina Grande (UFCG)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Semimonthly oscillation observed in the start times of equatorial
plasma bubbles",
journal = "Annales Geophysicae",
year = "2020",
volume = "38",
number = "2",
pages = "437--443",
month = "mar.",
abstract = "Using airglow data from an all-sky imager deployed at Sao Joao do
Cariri (7.4 degrees S, 36.5 degrees W), the start times of
equatorial plasma bubbles was studied in order to investigate the
day-to-day variability of this phenomenon. Data from a period over
10 years were analyzed from 2000 to 2010. Semimonthly oscillations
were clearly observed in the start times of plasma bubbles from
016300 airglow images during this period of observation, and four
case studies (September 2003, September-October 2005, November
2005 and January 2008) were chosen to show in detail this kind of
modulation. Since the airglow measurements are not continuous in
time, more than one cycle of oscillation in the start times of
plasma bubbles cannot be observed from these data. Thus, data from
a digisonde at Sao Luis (2.6 degrees S, 44.2 degrees W) in
November 2005 were used to corroborate the results.
Technical/climate issues did not allow one to observe the
semimonthly oscillations simultaneously by the two instruments,
but from October to November 2005 there was a predominance of this
oscillation in the start times of the irregularities over Brazil.
Besides, statistical analysis for the data in the whole period of
observation has shown that the lunar tide, which has semimonthly
variability, is likely the main forcing for the semimonthly
oscillation in the start times of equatorial plasma bubbles. The
presence of this oscillation can contribute to the day-to-day
variability of equatorial plasma bubbles.",
doi = "10.5194/angeo-38-437-2020",
url = "http://dx.doi.org/10.5194/angeo-38-437-2020",
issn = "0992-7689",
language = "en",
targetfile = "angeo-38-437-2020.pdf",
urlaccessdate = "28 abr. 2024"
}