“…In the past several decades, the main features of intracloud (IC) flashes and the incloud processes during cloud-to-ground (CG) flashes were resolved by the development of radio-based lightning mapping arrays operating at either high frequency/very high frequency (HF/VHF) [e.g., Proctor, 1981;Proctor et al, 1988;Mazur, 1989;Rhodes et al, 1994;Shao and Krehbiel, 1996;Rison et al, 1999;Kawasaki et al, 2000;Dong et al, 2002;Qiu et al, 2009;Zhang et al, 2010;Liu et al, 2012;Stock et al, 2014;Sun et al, 2014] or low frequency (LF) [e.g., Betz et al, 2004;Marshall et al, 2013;Bitzer et al, 2013;Karunarathne et al, 2013;Lyu et al, 2014;Yoshida et al, 2014;Wu et al, 2015;Wang et al, 2016]. A normal positive IC flash often starts with an initial negative leader that creates an upward channel bridging the negative and positive charge layers then horizontally extends into the two layers.…”