Positive cloud-to-ground (+CG) lightning flashes are less frequent than the negative counterpart, about 10% of the global cloud-to-ground lightning, but in general, their charge transfer is an order of magnitude greater (Rakov & Uman, 2003). For this reason, they usually can cause more damage, especially to tall structures like wind turbines (e.g., Becerra et al., 2018;Montanyà et al., 2014) or cause wildfire ignition (e.g., Blouin et al., 2016;Fuquay et al., 1972). Furthermore, +CG flashes are mainly associated with the production of transient luminous events like sprites (e.g., Boccippio et al., 1995;Williams et al., 2010). Therefore, +CG flashes have attracted significant research interest in recent years and some aspects are still debated or require a better understanding.One of these aspects concerns the origin and the development of multi-stroke +CG lightning. Positive flashes usually have a single stroke (Rakov & Uman, 2003). However, several cases of multi-stroke positive flashes were recently observed and reported in the literature. The first study reporting optical observations of multistroke +CG flashes was conducted by Fleenor et al. (2009). They documented for the first time subsequent positive strokes sharing the same channel to ground, and observed nine multi-stroke +CG flashes of which five cases involve a preexisting channel. Saba et al. (2010) reported high-speed video observations of 19 multi-stroke +CG flashes and only one case of subsequent positive stroke along the same channel. These optical observations highlighted the occurrence and rarity of the phenomenon, but present limitations in describing the flash development within the cloud and the mechanisms that make subsequent positive strokes possible.Thanks to improved lightning detection systems, new observations and findings on multi-stroke +CG flashes are emerging. Wu et al. (2020) reported 47 new observations during the winter season in Japan. They observe that downward positive leaders (DPLs) in multi-stroke flashes are mostly originated from in-cloud negative leader