How Does the Thermosphere and Ionosphere React to a Geomagnetic Storm

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Theoretical study of the low- and midlatitude ionospheric electron density enhancement during the October 2003 superstorm: Relative importance of the neutral wind and the electric field (2005, background): “Composition effects are also important, since the distribution of molecular nitrogen affects the recombination loss of the plasma [e.g., Rishbeth et al., 1987; Prölss, 1995; Fuller-Rowell et al., 1998].”
Global dayside ionospheric uplift and enhancement associated with interplanetary electric fields (2004, unknown): “Disturbance thermospheric winds associated with the disturbance dynamo processes could also cause significant modifications of the TEC at low and midlatitudes [Fuller-Rowell et al., 1997].”
Storm-time changes in the upper atmosphere at low latitudes (2002, background): “Many of the storm studies have focused on mid and high latitudes (Schunk and Sojka, 1996; Burns et al., 1991; Rishbeth et al., 1987; Fuller-Rowell et al., 1997; PrF olss, 1997), but there has been a growing interest in probing the response at low latitudes.”