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...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Teresa Barata, Joana Pereira, Manuel Hernández-Pajares, Tatiana Barlyaeva, Anna Morozova
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
TEC
Online Access:https://doi.org/10.3390/atmos14060949
https://doaj.org/article/3790e6eb6236496994143af330189909
Description
Summary: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.