Investigating the GIC index levels in the Mediterranean region during the strongest magnetic storms of solar cycle 25
- 1Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing (IAASARS), National Observatory of Athens (NOA), Penteli, Greece (zboutsi@noa.gr)
- 2Department of Physics, National and Kapodistrian University of Athens, Greece
- 3Hellenic Space Center, Athens, Greece
Geomagnetically Induced Currents (GICs) flowing along electrically conductive infrastructure, such as power transmission lines, are produced by a naturally induced geoelectric field during geomagnetic disturbances, such as magnetic storms. GICs can cause widespread blackouts across power grids, resulting in the loss of electric power. Although GIC intensity is greater in high latitudes, recent studies highlight the importance of considering GIC risks for countries located in the low and middle latitudes, including the Mediterranean region. GIC index is a proxy of the geoelectric field calculated entirely from geomagnetic field variations. Following a recent study where we investigated the GIC index levels for the Mediterranean (i.e., Greece, Italy, France, Spain, Algeria, and Turkey) for the most intense magnetic storms of solar cycle 24 (2008–2019), here we expand the analysis to encompass solar cycle 25. From the beginning of solar cycle 25 six major magnetic storms occurred with Dst index ≤ -100 nT. The three most intense magnetic storms (-163 nT < Dst < -212 nT) occurred in March, April and November 2023. We focus on those to compare with previous results showing that GIC index increases are well correlated with Storm Sudden Commencements (SSCs) and shed more light upon the expected GIC activity levels in the Mediterranean region during extreme events.
How to cite: Boutsi, A. Z., Balasis, G., Dimitrakoudis, S., Daglis, I. A., Tsinganos, K., Papadimitriou, C., and Giannakis, O.: Investigating the GIC index levels in the Mediterranean region during the strongest magnetic storms of solar cycle 25, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12696, https://doi.org/10.5194/egusphere-egu24-12696, 2024.