Equatorial Ionospheric Electric Fields During the November 2004 Magnetic Storm

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Super plasma fountain and equatorial ionization anomaly during penetration electric field (2009, background): “The vertical E B drift measured at Jicamarca (Figure 1a), which corresponds to the average drift over 200–600 km altitude [ Fejer et al., 2007 ], is applied to all field lines and hence to all altitudes and latitudes.”
A physical mechanism of positive ionospheric storms at low latitudes and midlatitudes (2010, background): “The drift velocities during the remaining period on the storm day are assumed to be equal to the quiet day values (thin curve) following Fejer et al. [2007] .”