Ionospheric F-Region Storms
By G. W. Prölss. 2017
281 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics
View Paper: https://www.semanticscholar.org/paper/3b50c921417d37562f158b95618c24c58ebc816f
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In Astronomy and Astrophysics
- Chaosong Huang
- A. Burns
- Elvira Astafyeva
- Huijun Le
- Irina Zakharenkova
- Wenbin Wang
- M. Förster
- Yongliang Zhang
In Geophysics
- Chaosong Huang
- A. Burns
- Elvira Astafyeva
- Irina Zakharenkova
- Wenbin Wang
- M. Förster
- Yongliang Zhang
- Shunrong Zhang
Citations in the corpus
- 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].”
- Ionospheric response to the 2015 St. Patrick's Day storm: A global multi‐instrumental overview (2015, background): “This, in turn, is the cause of both increases and decreases in electron plasma densities and total electron content (TEC), which are also known as positive and negative storms [Prölss, 1995; Richmond and Lu, 2000; Förster and Jakowski, 2000; Mendillo, 2006; Danilov, 2013].”
- A brief review of equatorial ionization anomaly and ionospheric irregularities (2018, background): “However, during later stages (or recovery phase RP) of the storms, the composition change effect of SEW becomes effective and positive ionospheric storms turn to negative storms (Prolss, 1995; Fuller-Rowell et al., 1994).”