Speaker
Description
Geomagnetic storms during the declining phase of the solar cycle 24 were studied using the total electron content (TEC) data obtained from three geodetic receivers located in Portugal: Lisbon (Continental Portugal), Furnas (Azores) and Funchal (Madeira). Two of the receivers (Lisbon and Furnas) are located at about the same latitude (~39ºN) while the third receiver (Funchal, ~33ºN) is positioned quite well to the south.
In this work, we study TEC variations during geomagnetic storms (Dst <= -50 nT) observed between 2015 and 2019. We draw conclusions on the strength type of the ionospheric response, and on the geomagnetic and other conditions that might favour a significant ionospheric storm in the studied region. Special attention is given to the analysis of the longitudinal and latitudinal (dis)similarities in the ionospheric variations, observed at the three studied locations.
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