“…MS waves can propagate both radially and azimuthally (e.g., Chen & Thorne,
2012; Hanzelka et al.,
2022; Kasahara et al.,
1994; Němec et al.,
2013; Santolík et al.,
2016; Xiao, Zhou, et al.,
2012), and across the plasmapause into the plasmasphere when excited outside of the plasmasphere (e.g., Liu et al.,
2018; Min et al.,
2019; Xiao, Zhou, et al.,
2015). MS waves can further propagate to extremely low L shells (
) (e.g., Miyoshi et al.,
2019; Yu et al.,
2021; Zhang et al.,
2021) with some even reaching the topside ionosphere observed by DEMETER (Detection of Electromagnetic Emissions Transmitted from Earthquake Regions) (e.g., Hanzelka et al.,
2022; Němec et al.,
2016; Santolík et al.,
2016). Geomagnetic field strength increases as MS waves propagate toward the Earth and the effects of heavy ions on the propagation start becoming important when the wave frequency becomes lower than the local proton cyclotron frequency.…”