Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms

The ionospheric response at middle latitudes to geomagnetic storms is not yet very well understood. Total electron content (TEC) variations associated with eight strong geomagnetic storms between 2015 and 2022 obtained from GNSS receivers in the eastern area of the North Atlantic (Portuguese contine...

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Published in:Atmosphere
Main Authors: Teresa Barata, Joana Pereira, Manuel Hernández-Pajares, Tatiana Barlyaeva, Anna Morozova
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
TEC
Online Access:https://doi.org/10.3390/atmos14060949
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spelling ftmdpi:oai:mdpi.com:/2073-4433/14/6/949/ 2023-08-20T04:08:16+02:00 Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms Teresa Barata Joana Pereira Manuel Hernández-Pajares Tatiana Barlyaeva Anna Morozova agris 2023-05-29 application/pdf https://doi.org/10.3390/atmos14060949 EN eng Multidisciplinary Digital Publishing Institute Upper Atmosphere https://dx.doi.org/10.3390/atmos14060949 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 6; Pages: 949 TEC geomagnetic storms middle latitudes GNSS Text 2023 ftmdpi https://doi.org/10.3390/atmos14060949 2023-08-01T10:16:18Z The ionospheric response at middle latitudes to geomagnetic storms is not yet very well understood. Total electron content (TEC) variations associated with eight strong geomagnetic storms between 2015 and 2022 obtained from GNSS receivers in the eastern area of the North Atlantic (Portuguese continental and insular territory) are studied in an attempt to fill this gap. It was found that for most of the studied geomagnetic storms, TEC variations are synchronous for the longitudinal ranges from 27° W and 9° W. In the southern part of the studied region (around 32° N), the amplitude of TEC variations is, in general, significantly higher than in the northern part (around 39° N). Some of the studied geomagnetic storms were associated with TEC variations that we interpret as effects of post-sunset equatorial plasma bubbles that travelled well north from their habitual region. Additionally, though most of the studied storms were accompanied by reports on different kinds of malfunction of GNSS systems (GPS; GALILEO and other), there is no clear pattern in their appearance in dependence on the geomagnetic/ionospheric storms’ strength, commencement time, and its characteristics, in general. Text North Atlantic MDPI Open Access Publishing Atmosphere 14 6 949
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic TEC
geomagnetic storms
middle latitudes
GNSS
spellingShingle TEC
geomagnetic storms
middle latitudes
GNSS
Teresa Barata
Joana Pereira
Manuel Hernández-Pajares
Tatiana Barlyaeva
Anna Morozova
Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms
topic_facet TEC
geomagnetic storms
middle latitudes
GNSS
description The ionospheric response at middle latitudes to geomagnetic storms is not yet very well understood. Total electron content (TEC) variations associated with eight strong geomagnetic storms between 2015 and 2022 obtained from GNSS receivers in the eastern area of the North Atlantic (Portuguese continental and insular territory) are studied in an attempt to fill this gap. It was found that for most of the studied geomagnetic storms, TEC variations are synchronous for the longitudinal ranges from 27° W and 9° W. In the southern part of the studied region (around 32° N), the amplitude of TEC variations is, in general, significantly higher than in the northern part (around 39° N). Some of the studied geomagnetic storms were associated with TEC variations that we interpret as effects of post-sunset equatorial plasma bubbles that travelled well north from their habitual region. Additionally, though most of the studied storms were accompanied by reports on different kinds of malfunction of GNSS systems (GPS; GALILEO and other), there is no clear pattern in their appearance in dependence on the geomagnetic/ionospheric storms’ strength, commencement time, and its characteristics, in general.
format Text
author Teresa Barata
Joana Pereira
Manuel Hernández-Pajares
Tatiana Barlyaeva
Anna Morozova
author_facet Teresa Barata
Joana Pereira
Manuel Hernández-Pajares
Tatiana Barlyaeva
Anna Morozova
author_sort Teresa Barata
title Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms
title_short Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms
title_full Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms
title_fullStr Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms
title_full_unstemmed Ionosphere over Eastern North Atlantic Midlatitudinal Zone during Geomagnetic Storms
title_sort ionosphere over eastern north atlantic midlatitudinal zone during geomagnetic storms
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/atmos14060949
op_coverage agris
genre North Atlantic
genre_facet North Atlantic
op_source Atmosphere; Volume 14; Issue 6; Pages: 949
op_relation Upper Atmosphere
https://dx.doi.org/10.3390/atmos14060949
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14060949
container_title Atmosphere
container_volume 14
container_issue 6
container_start_page 949
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