@Article{Romero-HernandezGoRoSeAgMeLu:2017:StIoDi,
author = "Romero-Hernandez, Esmeralda and Gonzalez-Esparza, J. Americo and
Rodriguez-Martinez, M. and Sergeeva, M. A. and Aguilar-Rodriguez,
Ernesto and Mejia-Ambriz, J. C. and De la Luz, V.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidad Nacional Aut{\'o}noma de M{\'e}xico} and
{Universidad Nacional Aut{\'o}noma de M{\'e}xico} and
{Universidad Nacional Aut{\'o}noma de M{\'e}xico} and
{Universidad Nacional Aut{\'o}noma de M{\'e}xico} and
{Universidad Nacional Aut{\'o}noma de M{\'e}xico} and
{Universidad Nacional Aut{\'o}noma de M{\'e}xico}",
title = "Study of ionospheric disturbances over Mexico associated with
transient space weather events",
journal = "Advances in Space Research",
year = "2017",
volume = "60",
number = "8",
pages = "1838--1849",
month = "Oct.",
keywords = "Ionospheric disturbancesDaytime ionospheric
scintillationGeomagnetic stormsSolar flares.",
abstract = "We present an analysis of ionospheric disturbances at a location
in Mexico (dip latitude: 28°, geographic latitude: 19° N) using
two different parameters: ionospheric scintillation (IONS) and
Total Electron Content (TEC). This study employs observations
during 20142015 of astronomical radio sources at 140 MHz obtained
by the MEXican Array Radio Telescope (MEXART) and TEC values from
Global Ionospheric Maps data. To identify the ionospheric
disturbances two indices were used: the wavelet IONS index based
on the wavelet transform function of MEXART data and the
ionospheric W-index based on the deviation of TEC. A set of 55
wavelet IONS events and 63 W-index events were identified in this
interval. We analyzed the association of theses events with solar
flares that occurred around the solar zenith and/or geomagnetic
storms. During this period, it was observed an incidence of
daytime IONS at hours around the solar zenith. Some possible
associations with solar flares were found. The preliminary results
pointed out that, for this period, daytime scintillations could be
linked to the occurrence of Esb-layers. In addition, most of the
W-index events were possibly related to geomagnetic storms. We
found that the majority of these geomagnetic storms were minor and
moderate storms and were characterized by steeper falls of Dst.
This first analysis revealed that wavelet methodology is useful in
identifying and analyzing ionospheric disturbances. Also, MEXART
observations provide a good tool for performing IONS studies at
mid latitudes.",
doi = "10.1016/j.asr.2017.06.042",
url = "http://dx.doi.org/10.1016/j.asr.2017.06.042",
issn = "0273-1177 and 1879-1948",
language = "en",
targetfile = "esmeralda_study.pdf",
urlaccessdate = "24 abr. 2024"
}