“…[2] The coupling between the magnetosphere and the ionosphere through precipitating particles from radiation belts and the central plasma sheet that strongly controls ionization and conductance in the ionosphere has been known for some time, although it is one of the most difficult couplings to understand [e.g., Paulikas, 1975;Buonsanto, 1999;Ma et al, 2008;Kelley, 2009]. The energy deposition of precipitating particles of various energies mainly through the ionization of atmospheric atoms occurs at different altitudes, particularly within the D, E, and F regions of the ionosphere and extends from high to midlatitudes and over the South-Atlantic Anomaly (SAA) at low latitudes [e.g., Voss and Smith, 1980;Vampola and Gorney, 1983;Rees et al, 1988;Abel et al, 1997]. An impact of precipitating particles in the lower ionosphere (the D and E layers) and the upper atmosphere in terms of enhanced ionization and other related aeronomical effects has been investigated in a large number of studies [e.g., Buonsanto, 1999, and references therein;Nishino et al, 2002;Peter et al, 2006;Clilverd et al, 2008Clilverd et al, , 2010Turunen et al, 2009;Lam et al, 2010;Dmitriev et al, 2011], while evidence for ionospheric signatures in the topside ionosphere (F region) in the midlatitudes and over the SAA at low latitudes have also been reported [e.g., Foster et al, 1994Foster et al, , 1998Abdu et al, 2005;Kunitsyn et al, 2008aKunitsyn et al, , 2008bDmitriev and Yeh, 2008;Pedatella et al, 2009;Ngwira et al, 2012].…”