“…Ground-based facilities, such as ionosonde stations, magnetic observatories and GPS receivers can monitor various parameters used to detect ionospheric anomalies, such as F2-layer critical frequency (foF2), total electron content (TEC), electron temperature (Te) at F2-layer heights, magnetic pulsations and low-frequency radio signals (see, e.g., Hayakawa et al, 1999;Strakhov and Liperovsky, 1999;Bortnik et al, 2008;Ondoh, 2009;Trigunait et al, 2004;Hobara and Parrot, 2005;Liu et al, 2006;Maekawa et al, 2006;Sharma et al, 2006;Ondoh and Hayakawa, 2006;Dabas et al, 2007;Oikonomou et al, 2016).…”