@Article{SousasantosAbSaBaSiLo:2020:CoLoOb,
author = "Sousasantos, Jonas and Abdu, Mangalathayil Ali and Santos, Angela
and Batista, Inez Staciarini and Silva, Andr{\'e} and Loures,
Luis Eduardo",
affiliation = "{Instituto Tecnol{\'o}gico de Aeron{\'a}utica (ITA)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Tecnol{\'o}gico de
Aeron{\'a}utica (ITA)} and {Instituto Tecnol{\'o}gico de
Aeron{\'a}utica (ITA)}",
title = "Further complexities on the pre-reversal vertical drift modeling
over the Brazilian region: a comparison between long-term
observations and model results",
journal = "Journal of Space Weather and Space Climate",
year = "2020",
volume = "10",
pages = "e2020022",
keywords = "Pre-reversal vertical drift / Equatorial plasma electrodynamics /
Ionospheric modeling.",
abstract = "The vertical component of the plasma drift, especially the
evening-time pre-reversal drift, constitutes an important aspect
of the nighttime electrodynamics of the equatorial ionosphere.
Over the years, several studies using measurements and models have
been performed to understand the characteristics of this process
and its implications for the development of the instabilities
leading to the plasma bubble formation and ionospheric
scintillation. However, the Brazilian region presents some unique
features that bring some difficulties for the vertical drift
prognosis, which is required for the scintillation forecasting.
These features are mainly related to the geomagnetic field lines
topology that presents strong differences when compared to those
of other equatorial longitudes. In this work, some of the
difficulties for the prereversal vertical drift modeling and
estimation are discussed; also, a dataset containing long-term
observation (20012009) is compared with a widely used empirical
model. The results show an intrinsic trend of underestimation by
the model, which seems to be independent of latitude and
seasonality thus suggesting an additional contribution arising
from sources other than solely the geomagnetic topology. Also, the
results indicate that the deviation can vary in the range of 040
m/s and the percentage error enhances with increasing values of
pre-reversal vertical drift peak and reduces with increasing F10.7
values, thereby, indicating a clear possibility of meridional
winds contribution which is not included in the empirical model
used and may account for these differences.",
doi = "10.1051/swsc/2020022",
url = "http://dx.doi.org/10.1051/swsc/2020022",
issn = "2115-7251",
language = "en",
targetfile = "Sousasantos_Further.pdf",
urlaccessdate = "25 abr. 2024"
}