@Article{AbduSRGHRCSB:1996:ZoWiDi,
author = "Abdu, Mangalathayil Ali and Sobral, Jos{\'e} Humberto Andrade and
Richards, P. and Gonzalez, Marta M. de and Huang, Y. N. and Reddy,
B. M. and Cheng, K. and Szuszczewicz, E. P. and Batista, Inez
Staciarini and 26729-26740",
title = "Zonal/meridional wind and disturbance dynamo electric field
control of the low-latitude ionosphere based on the SUNDIAL/ATLAS
1 Campaign",
journal = "Journal of Geophysical Research",
year = "1996",
volume = "101",
number = "A12",
month = "dec.",
keywords = "AERONOMIA, perturbacoes ionosf{\'e}ricas, campos eletricos,
regioes tropicais (baixa latitude), ionospheric distrurbances,
eletric fields, tropical regions (low latitudes).",
abstract = "We present an evaluation of global-scale equatorial and low
latitude ionospheric disturbances in response to the
weak-to-moderate disturbed conditions that marked the
SUNDIAL/ATLAS1 twelve-day campaign of March 22 to April 2, 1992.
Ionosonde data from South American and Indian-Asian longitudes are
analyzed to examine first the climatological (the average) pattern
of the critical F region parameters (the layer peak density and
height) in comparison with the empirical International Reference
Ionospheric model, and then to characterize the day-to-day
variabilities aiming at identifying potential causal contributions
from either disturbance zonal and meridional winds or
magnetospheric, and disturbance dynamo electric fields. Included
in this analysis are data from South American midlatitude
locations which are used to determine meridional winds using an
adaptation of the servo analysis technique in the Field Line
Integrated Plasma (FLIP) model. We have made an assessment of the
causal mechanism of the day-to-day variabilities as arising from
latitude dependent disturbance meridional winds, and from electric
fields produced by disturbance zonal winds and disturbance dynamo.
While the contribution from disturbance meridional winds decreases
from middle to equatorial latitudes, that of the electric fields
maximizes around the equator. In particular, first-time evidence
based on ionosonde data is provided for a disturbance dynamo
electric field in the equatorial ionosphere. It is found that
there are two time intervals of maximum ionospheric variability
resulting from the weak to moderate magnetospheric; disturbance
conditions that prevailed during the campaign: one near the
evening/postsunset hours and the other in the postmidnight-sunrise
hours over low latitudes. At midlatitudes a broad maximum of the
response occurs from premidnight to morning hours. We provide a
comparison of results for the South American and Indian-Asian
longitudes and a discussion of the competing roles of the
disturbance zonal and meridional winds, and magnetospheric and
disturbance dynamo electric fields as a function of latitude.",
issn = "0148-0227 and 2156-2202",
label = "8098",
targetfile = "8399.pdf",
urlaccessdate = "08 maio 2024"
}