“…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) …”