A strong positive phase of ionospheric storms observed by the Millstone Hill incoherent scatter radar and global GPS network

By Chaosong Huang, J. Foster, L. P. Goncharenko, Philip J. Erickson, W. Rideout, Anthea J. Coster. 2005

133 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/89bac789c52d65a7ddb2c0542210c7af9e1cd484

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In Aerospace Engineering

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Citations in the corpus

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): “…that the midlatitude ionosphere may be influenced as the EIA expands poleward and become most highly pronounced during the early stage of a major magnetic storm [e.g., Tanaka, 1986; Abdu, 1997; Basu et al., 2001; Vlasov et al., 2003; Tsurutani et al., 2004; Huang et al., 2005; Lin et al., 2005].”
Profiles of ionospheric storm‐enhanced density during the 17 March 2015 great storm (2015, background): “Positive ionospheric storm effects can be of short (<6 h) or long duration (longer than 6 h) [e.g., Bauske and Prolss, 1997; Huang et al., 2005].”
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].”
Long‐duration penetration of the interplanetary electric field to the low‐latitude ionosphere during the main phase of magnetic storms (2005, methodology): “As reported in detail by Huang et al. [2005] , the midlatitude ionospheric F peak moved upward rapidly during the interval of southward IMF, and the electron density was increased by a factor of 2–4 over the F region compared to the previous quiet-time values.”
GPS observations of the ionospheric F2-layer behavior during the 20th November 2003 geomagnetic storm over South Korea (2008, background): “The significant increases of F2-layer peak height and density last for about 10 h and is classified as a long-duration ionospheric positive storm (Huang et al. 2005a).”