@Article{AbduBRSSPMSPG:2009:ElHiSp,
author = "Abdu, Mangalathayil Ali and Batista, Inez Staciarini and Reinisch,
B. W. and Souza, J. R. de and Sobral, Jose Humberto Andrade and
Pedersen, T. R. and Medeiros, A. F. and Schuch, Nelson Jorge and
Paula, Eurico Rodrigues de and Groves, K. M.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Center for
Atmospheric, University of Massachusettes, Lowell, USA and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Air Force Research
Laboratoy, Hanscom Air Force Base, Massachusetts, USA and
{Universidade Federal de Campina Grande. Brazil} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and Air Force Research Laboratoy,
Hanscom Air Force Base, Massachusetts, USA",
title = "Conjugate point equatorial experiment (COPEX) campaign in Brazil:
Eletrodynamics hightlights on spread F development conditions and
day-to-day variability",
journal = "Journal of Geophysical Research",
year = "2009",
volume = "114",
number = "A04308",
month = "Apr.",
keywords = "Conjugate ionospheres, plasma bubble/spread F, vertical plasma
drift, transequatprial wind, large scale wave structures, ESF
day-to-day variability.",
abstract = "A conjugate point equatorial experiment (COPEX) campaign was
conducted during October - December 2002 period in Brazil, with
the objective to investigate the equatorial spread F/plasma bubble
irregularity (ESF) development conditions in terms of the
electrodynamical state of the ionosphere along the magnetic flux
tubes in which they occur. A network of instruments including
digisondes, optical imagers, and GPS receivers, were deployed at
magnetic conjugate and dip equatorial locations, in a geometry
that permitted field line mapping of the conjugate E layers to dip
equatorial F layer bottomside. We analyze in this paper the
extensive digisonde data from the COPEX stations, complemented by
limited all-sky imager conjugate point observations. The SUPIM
(Sheffield University Plasmasphere-ionosphere Model) is used to
assess the transequatorial winds (TEW) as inferred from the
observed difference of hmF2 at the conjugate sites. New results
and evidences on the ESF development conditions and the related
ambient electrodynamic processes from this study can be
highlighted as follows: 1) large scale bottomside wave
structures/satellites traces at equator followed by their
simultaneous appearance at conjugate sites are shown to be
indicative of the ESF instability initiation; 2) the evening
prereversal electric field enhancement (PRE)/vertical drift
presents systematic control on the time delay in SF onset at
off-equatorial sites indicative of the vertical bubble growth,
under weak transequatorial wind; 3) the PRE presents large
latitude/height gradient in the Brazilian sector; 4) conjugate
point symmetry/asymmetry of large scale plasma depletions versus
smaller scale structures are revealed; 5) while transequatorial
winds seem to suppress ESF development in a case study, the medium
term trend in the ESF seems to be controlled more by the variation
in the PRE than in the TEW during the COPEX period. Competing
influences of the evening vertical plasma drift in favoring the
ESF development and that of the TEW in suppressing its growth are
discussed presenting a perspective on the ESF day-to-day and
medium term variabilities.",
doi = "10.1029/2008JA013749",
url = "http://dx.doi.org/10.1029/2008JA013749",
issn = "0148-0227 and 2156-2202",
language = "en",
targetfile = "Conjugate point equatorial experiment (COPEX) campain in Brazil
Electrodynamics highlights on spread F... M. A. Abdu.pdf",
urlaccessdate = "13 maio 2024"
}