2017
DOI: 10.1016/j.asr.2016.11.039
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Ion density variation at upper ionosphere during thunderstorm

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Cited by 4 publications
(3 citation statements)
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“…Nowadays increasing and emerging evidences are pointing to the close link between the upper atmosphere (e.g., the positive plate) and lower atmosphere (e.g., the negative plate) [Harrison et al, 2010;Rycroft, 2006]. For example, thunderstorm occurring in the lower atmosphere is suggested to have a direct impact on the ES layer based on recent observational results [Bortnik et al, 2006;Christos, 2018;Cummer et al, 2009;Curtius et al, 2006;Davis and Johnson, 2005;Davis and Lo, 2008;England et al, 2006;Fukunishi et al, 1996;Girish and Eapen, 2008;Haldoupis et al, 2012;Immel et al, 2013;Kumar et al, 2009;Kuo and Lee, 2015;Lay et al, 2015;Mangla et al, 2016;Maruyama, 2006;Pasko et al, 2002;Rodger et al, 2001;Rycroft, 2006;Sátori et al, 2013;Sentman and Wescott, 1995;Shao et al, 2013;Sharma et al, 2004;Su et al, 2003;Surkov et al, 2006;Yu et al, 2015] or even the sodium layer [Yu et al, 2017]. The possible carriers or phenomena connecting the thunderstorm to the upper atmosphere are suggested to be atmospheric tides [England et al, 2006;Haldoupis et al, 2004;Immel et al, 2013], planetary waves [Lv et al, 2004], gravity waves [Davis and Johnson, 2005;Kumar et al, 2009;Lay et al, 2015;Shao et al, 2013], transient luminous event (TLEs) …”
mentioning
confidence: 99%
“…Nowadays increasing and emerging evidences are pointing to the close link between the upper atmosphere (e.g., the positive plate) and lower atmosphere (e.g., the negative plate) [Harrison et al, 2010;Rycroft, 2006]. For example, thunderstorm occurring in the lower atmosphere is suggested to have a direct impact on the ES layer based on recent observational results [Bortnik et al, 2006;Christos, 2018;Cummer et al, 2009;Curtius et al, 2006;Davis and Johnson, 2005;Davis and Lo, 2008;England et al, 2006;Fukunishi et al, 1996;Girish and Eapen, 2008;Haldoupis et al, 2012;Immel et al, 2013;Kumar et al, 2009;Kuo and Lee, 2015;Lay et al, 2015;Mangla et al, 2016;Maruyama, 2006;Pasko et al, 2002;Rodger et al, 2001;Rycroft, 2006;Sátori et al, 2013;Sentman and Wescott, 1995;Shao et al, 2013;Sharma et al, 2004;Su et al, 2003;Surkov et al, 2006;Yu et al, 2015] or even the sodium layer [Yu et al, 2017]. The possible carriers or phenomena connecting the thunderstorm to the upper atmosphere are suggested to be atmospheric tides [England et al, 2006;Haldoupis et al, 2004;Immel et al, 2013], planetary waves [Lv et al, 2004], gravity waves [Davis and Johnson, 2005;Kumar et al, 2009;Lay et al, 2015;Shao et al, 2013], transient luminous event (TLEs) …”
mentioning
confidence: 99%
“…Nowadays increasing and emerging evidence is pointing to the close link between the upper atmosphere (e.g., the positive plate) and lower atmosphere (e.g., the negative plate) (Harrison et al, 2010;Rycroft, 2006). For example, a thunderstorm occurring in the lower atmosphere is suggested to have a direct impact on the E S layer based on recent observational results (Bortnik et al, 2006;Christos, 2018;Cummer et al, 2009;Curtius et al, 2006;Davis and Johnson, 2005;Davis and Lo, 2008;England et al, 2006;Fukunishi et al, 1996;Girish and Eapen, 2008;Haldoupis et al, 2012;Immel et al, 2013;Kumar et al, 2009;Kuo and Lee, 2015;Lay et al, 2015;Mangla et al, 2016;Maruyama, 2006;Pasko et al, 2002;Rodger et al, 2001;Rycroft, 2006;Sátori et al, 2013;Sentman and Wescott, 1995;Shao et al, 2013;Sharma et al, 2004;Su et al, 2003;Surkov et al, 2006;Yu et al, 2015) or even on the sodium layer (Yu et al, 2017). The possible carriers or phenomena connecting the thunderstorm to the upper atmosphere are suggested to be atmospheric tides (England et al, 2006;Haldoupis et al, 2004;Immel et al, 2013), planetary waves (Lv et al, 2004), gravity waves (Davis and Johnson, 2005;Kumar et al, 2009;Lay et al, 2015;…”
Section: Introductionmentioning
confidence: 99%
“…The separation of charges in the thundercloud may eventually produce an electric field that becomes so large (around 3 × 10 5 ∼ 4 × 10 5 V m −1 ) that it could initiate the lightning stroke [5]. One fact agreed by most of researchers [6][7][8][9][10][11][12] is the contribution of intense lightning discharges to the global electric circuit (GEC). The substantial role of the lightning and thunderstorm in GEC would justify the need to investigate the charge structure of thunderclouds.…”
Section: Introductionmentioning
confidence: 99%