Among the different types of lighting that occur on Earth, the cloud-to-ground (CG) lightning is the one most studied and investigated phenomenon because of its real threat to human beings, electric power systems, telecommunication systems, and electrical and electronic systems in general. The downward CG flashes consist of a single return-stroke (RS) or a first RS, followed by several subsequent strokes (SS). The CG lightning flash usually involves a preliminary breakdown (PB) process followed by a downward leader and a RS that connects to the ground during the attachment process. In negative RS, negative charge is effectively transported to the ground, and in positive RS, the opposite charge transfer occurs (Uman, 1987). The incidence of CG flashes is estimated to be 25% of all lightning occurrences on Earth (Rakov, 2016;Rakov & Uman, 2003). In the U.S, according to Medici et al. (2017), the incidence of CG flashes varies from 15% to 44%. The characteristics of CG lightning are in the field of interest for engineering applications, geophysical research, meteorology, among other fields of study.It is known that lightning parameters can vary from one storm to another (Saraiva et al., 2010;Y. Zhu, Rakov et al., 2015). Also, lightning parameters can change from one region to another region of the globe due to the regional physiography and atmospheric conditions (Kilinc & Beringer, 2007;Kuleshov, 2004;Mushtaq et al., 2018) and, mainly regarding different latitudes (Pinto et al., 1997;Thomson, 1980b). However, Thomson (1980b) suggested that those differences could be because of the different methodologies employed to measure the parameters, for instance, different sample rates of digitizers, different trigger thresholds, and different equipment in general. Recently, Cooray et al. (2020), developed a theory to explain why the peak current in negative return strokes increases as the latitude decreases. They showed that this dependence is related to the difference in the heights of the charge centers in the thunderclouds at different geographical regions. The Amazon region is located in the low latitude region, and so, high-intensity lightning flashes are expected. Those high-intensity CG flashes were observed by Almeida et al. (2012) in the eastern Amazon region.