@Article{BalanSouzBail:2018:ReDeUn,
author = "Balan, Nalan and Souza, Jonas Rodrigues de and Bailey, G. J.",
affiliation = "{University of Sheffield} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {University of Sheffield}",
title = "Recent developments in the understanding of equatorial ionization
anomaly: a review",
journal = "Journal of Atmospheric and Solar-Terrestrial Physics",
year = "2018",
volume = "171",
pages = "3--11",
month = "June",
keywords = "Review, Recent developments, Equatorial ionization anomaly, Quiet
and active conditions, Super plasma fountain, Strong anomaly.",
abstract = "A brief review of the recent developments in the understanding of
the equatorial plasma fountain (EPF) and equatorial ionization
anomaly (EIA) under quiet and active conditions is presented. It
is clarified that (1) the EPF is not upward ExB plasma drift at
the equator followed by downward plasma diffusion, but it is field
perpendicular ExB plasma drift and field-aligned plasma diffusion
acting together all along the field lines at all altitudes and
plasma flowing in the direction of the resultant. (2) The EIA is
formed not from the accumulation of plasma at the crests but
mainly from the removal of plasma from around the equator by the
upward ExB drift with small accumulations when the crests are
within approximately ±20° magnetic latitude. The accumulations
reduce with increasing latitude and become zero by approximately
±25°. (3) An asymmetric neutral wind makes EPF and EIA asymmetric
with stronger fountain and stronger crest usually occurring in
opposite hemispheres especially at equinoxes when winter anomaly
is absent. (4) During the early stages of daytime main phase of
major geomagnetic storms, the plasma fountain becomes a super
fountain and the EIA becomes strong not due to the eastward prompt
penetration electric field (PPEF) alone but due to the combined
effect of eastward PPEF and storm-time equatorward winds (SEW).
(5) During the later stages of the storms when EIA gets inhibited
a peak sometimes occurs around the equator not due to westward
electric fields but mainly due to the convergence of plasma from
both hemispheres due to SEW.",
doi = "10.1016/j.jastp.2017.06.020",
url = "http://dx.doi.org/10.1016/j.jastp.2017.06.020",
issn = "1364-6826",
language = "en",
targetfile = "balan_recent.pdf",
urlaccessdate = "27 abr. 2024"
}