Braided rivers constitute fluvial systems of high morphological complexity and significant geomorphologicaldynamism. This study analyses the morphological dynamics and braiding intensity of the San Carlo reachof the Fiumara Amendolea for the period 2022–2024. The Fiumara presents optimal characteristics for thedevelopment of the braiding model: it is a short, steep, ephemeral and torrential watercourse with scarce riparianvegetation. The analysis of braided systems, such as the one studied here, is key in the context of climatechange, where an increase in the frequency of extreme precipitation events is expected. For the analysed period,a simplification of the network is observed, a phenomenon that can be attributed to torrential precipitationepisodes recorded during the study period. The methodology integrates photogrammetric processing usingStructure from Motion (SfM) of multispectral UAV/RPAS surveys, GIS-based spatial analysis, and automatedchannel network extraction using RivGraph. To measure braiding intensity, four braiding indices (BI) —Brice,Germanoski-Schumm, Mosley, and the Entropic Braiding Index (eBI; Tejedor et al., 2022)— were computedfor each sub-reach of both the full channel and the most active reach. Additionally, a series of morphologicalindices and variables were calculated to establish correlation relationships with the BIs, in order to determinewhich of these is most representative of the spatial reality of the Fiumara Amendolea. The results reveal ageneralised reduction pattern in braiding intensity over the analysed period, with alternation of the dominantgeomorphological process; in the headward sector of the San Carlo reach, sedimentation prevails, whereasincision dominates downstream.Keywords: braided channels, BI, eBI, Amendolea Fiumara, fluvial geomorphology, SfM photogrammetry,multitemporal analysis.