Upper-atmospheric effects of magnetic storms: a brief tutorial

By Arthur D. Richmond, G. Lu. 2000

200 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/71b80b713c4a1731a3543feb7da987da26188901

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Citations in the corpus

Ionospheric response to the 2015 St. Patrick's Day storm: A global multi‐instrumental overview (2015, background): “…fields, as well as plasmaspheric downward fluxes, have been reported to be the main causes of the storm time increases in the ionospheric plasma density [e.g., Fuller-Rowell et al., 1996; Richmond and Lu, 2000; Förster and Jakowski, 2000; Huang et al., 2005; Crowley et al., 2006; Danilov, 2013].”
Dayside global ionospheric response to the major interplanetary events of October 29–30, 2003 “Halloween Storms” (2005, background): “[2] The ionospheric response to changes in solar wind conditions has been the subject of concerted study for several decades [Blanc and Richmond, 1980; Prolss, 1997; Buonsanto, 1999; Richmond and Lu, 2000; FullerRowell et al., 1997].”
Profiles of ionospheric storm‐enhanced density during the 17 March 2015 great storm (2015, background): “…wind convergence, penetration and disturbance dynamo electric fields, downward plasma flux from the plasmasphere, traveling atmospheric disturbances (TADs), and auroral particle precipitation [Prölss, 1995; Buonsanto, 1999; Richmond and Lu, 2000, Mendillo, 2006; Burns et al., 2007; Danilov, 2013].”
Global dayside ionospheric uplift and enhancement associated with interplanetary electric fields (2004, unknown): “…et al., 2003], following the early theoretical work of Blanc and Richmond [1980], and/or (2) delayed electric fields produced by the disturbance dynamo driven by Joule heating due to storm energy input at high latitudes [Blanc and Richmond, 1980; Richmond and Lu, 2000; Scherliess and Fejer, 1997].”
Magnetospheric disturbance induced equatorial plasma bubble development and dynamics: A case study in Brazilian sector (2003, background): “…the storm energy input at high latitudes produces a global scale disturbance thermospheric circulation and the action of Coriolis force imparts a westward momentum to this, resulting in westward directed winds gaining importance at middle latitudes [Blanc and Richmond, 1980; Richmond and Lu, 2000].”