@Article{EssienFTKWAQLASESSBNQ:2022:InCoZo,
author = "Essien, Patrick and Figueiredo, Cosme Alexandre Oliveira Barros
and Takahashi, Hisao and Klutse, Nana Ama Browne and Wrasse,
Cristiano Max and Afonso, Jo{\~a}o Maria de Sousa and Quispe,
David Pareja and Lomotey, Solomon Otoo and Ayorinde, Tunde Toyese
and Sobral, Jos{\'e} Humberto Andrade and Eghan, Moses Jojo and
Sackey, Samuel Sanko and Silva, Diego Barros and Bilibio, Anderson
Vestena and Nkrumah, Francis and Quagraine, Kwesi Akumenyi",
affiliation = "{University of Cape Coast} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {African Institute for Mathematical Sciences (AIMS)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{National Institute of Meteorology and Geophysics of Angola
(INAMET)} and {Universidad Nacional Mayor de San Marcos (UNMSM)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {University of Cape
Coast} and {University of Cape Coast} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {University of Cape Coast} and {University
of Cape Coast}",
title = "Intertropical Convergence Zone as the Possible Source Mechanism
for Southward Propagating Medium-Scale Traveling Ionospheric
Disturbances over South American Low-Latitude and Equatorial
Region",
journal = "Atmosphere",
year = "2022",
volume = "13",
number = "11",
pages = "e1836",
month = "Nov",
keywords = "gravity waves, ionosphere, ITCZ, MSTIDs.",
abstract = "This paper presents the Intertropical Convergence Zone (ITCZ) as
the possible source mechanism of the medium-scale traveling
ionospheric disturbances (MSTIDs) propagating to the southeast
direction over the South American region. Using the data collected
by the GNSS dual-frequency receivers network from January 2014 to
December 2019, detrended TEC maps were generated to identify and
characterize 144 MSTIDs propagating southeastward over the South
American low-latitude and equatorial region. We also used images
from the Geostationary Operational Environmental Satellite (GOES)
13 and 16 in the infrared (IR) and water vapor (WV) channel, and
reanalisys data from the National Centers for Environmental
Prediction (NCEP) of the National Oceanic and Atmospheric
Administration (NOAA) to study the daily features and seasonal
migration of ITCZ. In the winter, when ITCZ migrates to the
northern hemisphere around 1015° N, 20 MSTIDs propagated
southeastward. During summer, when the ITCZ lies within the
continent, around 05° S 80 MSTIDs were observed to propagate
southeastward; in the equinoxes (spring and fall), 44 MSTIDs were
observed. Again, the MSTIDs propagating southeastward showed a
clear seasonality of their local time dependence; in summer, the
MSTIDs occurred frequently in the evening hours, whereas those in
winter occurred during the daytime. We also found for the first
time that the day-to-day observation of ITCZ position and MSTIDs
propagation directions were consistent. With regard to these new
findings, we report that the MSTIDs propagating southeastward over
the South American region are possibly induced by the atmospheric
gravity waves, which are proposed as being generated by the ITCZ
in the troposphere. The mean distribution of the horizontal
wavelength, period, and phase velocity are 698 ± 124 km, 38 ± 8
min, and 299 ± 89 m s\−1, respectively. For the first time,
we were able to use MSTID propagation directions as a proxy to
study the source region.",
doi = "10.3390/atmos13111836",
url = "http://dx.doi.org/10.3390/atmos13111836",
issn = "2073-4433",
language = "en",
targetfile = "atmosphere-13-01836.pdf",
urlaccessdate = "04 maio 2024"
}