@Article{FagundesSahaBittTaka:1995:ReGeEq,
author = "Fagundes, Paulo Roberto and Sahai, Yogeshwar and Bittencourt, Jose
Augusto and Takahashi, Hisao",
title = "Relationship between generation of the equatorial F-region plasma
bubbles and thermospheric dynamics",
journal = "Advances in Space Research",
year = "1995",
volume = "16",
number = "5",
pages = "117--120",
keywords = "AERONOMIA, bolhas de plasma, termosfera, din{\^a}micas, ondas
gravitacionais, regi{\~a}o F, irregularidades,
propaga{\c{c}}{\~a}o F, plasma bubbles, spread F, thermosphere,
dynamics, gravity waves, irregularities.",
abstract = "Simultaneous zenith measurements of the OI 630.0 nm and 557.7 nm
nightglow emissions, using a multi-channel tilting filter type
photometer and nighttime thermospheric neutral wind velocities
from the Doppler shifts of the OI 630.0 nm emission line, using a
Fabry-Perot interferometer, have been carried out at Cachoeira
Paulista (23 degrees S, 45 degrees W), Brazil, during 1988-1991.
These measurements constitute a unique opportunity to study the
relationship between the generation of F-region plasma bubbles
(regions of depleted electron densities) and thermospheric
dynamics. During the period of March 1988 to June 1991, we have 9
nights on which there were nearly full nights of simultaneous
observations of thermospheric wind velocities (zonal and
meridional) and the OI 630.0 nm and 557.7 nm emissions showing
formation of plasma bubbles. On the night of March 18, 1991, the
zonal wind was unusually strong in the beginning of the night (300
m/s) and this night shows very strong formation of plasma bubbles,
indicating that a strong zonal wind in some way may be connected
with plasma bubble formation through the electric field created by
the interaction between the zonal wind and the Earth's magnetic
field. However, both the zonal and meridional winds on several
nights with, and without plasma bubbles, are comparable. This
feature possibly indicates only a secondary role of thermospheric
winds in the generation of the equatorial ionospheric plasma
depletions. It should be pointed out that an analysis of the
nocturnal intensity variations of simultaneous mesospheric
(E-region) emissions (O1 557.7 nm, O-2 atm. 864.5 nm, NaD 589.0 nm
and OH (9-4) 775.0 nm) on all the nine nights studied, shows the
presence of gravity waves, indicating possible relation between
wave processes in the mesosphere and F-region irregularities.",
issn = "0273-1177",
label = "7145",
language = "en",
targetfile = "1-s2.0-027311779500180M-main.pdf",
urlaccessdate = "12 maio 2024"
}