@Article{CandidoBaBeAbSoTa:2011:SpOcOv,
author = "Candido, Cl{\'a}udia Maria Nicoli and Batista, Inez Starciarini
and Becker-Guedes, F{\'a}bio and Abdu, Mangalahyil Ali and
Sobral, Jos{\'e} Humberto de Andrade and Takashi, Hisao",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "Spread F occurrence over a southern anomaly crest location in
Brazil during June solstice of solar minimum activity",
journal = "Journal of Applied Geophysics",
year = "2011",
volume = "116",
pages = "AO6316.",
month = "Jun 24",
keywords = "VERTICAL PLASMA DRIFTS, AMERICAN SECTOR, LOW LATITUDES,
EQUATORIAL, REGION, IRREGULARITIES, DISTURBANCES, DEPLETIONS,
SATELLITE, BUBBLES.",
abstract = "We present a study of Spread F occurrence over a location under
the southern crest of the equatorial ionization anomaly (Cachoeira
Paulista 22.7 degrees S, 45.0 degrees W, mag. Lat.: 16 degrees S,
dip angle: -32.3 degrees, Brazil) during the last solar cycle,
which presented an extended solar minimum activity. After
analyzing hundreds of ionograms obtained with a digital ionosonde
DGS 256, between 2001 and 2010, we verified high Spread F
occurrence around midnight-postmidnight during June solstice
(Southern Hemisphere winter) with a peak occurrence between 2006
and 2009, when the solar flux has reached very low values (<70
SFU). At the Brazilian sector the occurrence of Spread F is known
to be associated with equatorial plasma bubbles (EPBs) and is
observed mainly between September and March. On the other hand,
EPBs are rarely observed over Cachoeira Paulista (hereafter
referred as CP) during June solstice because of the weak
magnitudes of the equatorial electric field prereversal
enhancement, an essential condition to the development of the
large-scale irregularities at the equatorial region. Despite the
rarity of EPBs, we observed several strong Spread F events
occurring under low plasma densities conditions which can extend
for several hours. We have found evidences that the Spread F
events over CP during June solstices of low solar activity can be
caused by ionospheric disturbances that are unrelated to
equatorial processes. Finally we present a statistical analysis of
the events and we suggest that traveling ionospheric disturbances
could be one of the main sources of these nonequatorial Spread F
events.",
doi = "10.1029/2010JA016374",
url = "http://dx.doi.org/10.1029/2010JA016374",
issn = "0926-9851",
language = "en",
urlaccessdate = "01 maio 2024"
}