The spatial distribution of charge plays a crucial role during lightning development (Iudin et al., 2017;Zheng et al., 2019). A typical thunderstorm cloud has a three-layer charge structure: a positive charge region at the top, a negative charge region in the middle and a small positive charge region at the bottom (Krehbiel, 1986;Williams et al., 1985). At present, the vertical layered structure is mainly used in research to reveal the propagation behavior of lightning (Krehbiel, 2003;Nag & Rakov, 2009;Qie, 2005). However, a growing body of research suggests that the charge structure of thunderstorm clouds is more complex (Stolzenburg et al., 1998) and possibly manifests itself as a staggering of more charge regions, and the horizontal extent of the charge regions can often be much larger than the vertical extent (