Large wood (LW) is recruited into river systems either through incremental or chronic processes, such as attributed to tree mortality and bank undercutting, or through episodic processes (i.e., flood events, landslides, windthrow, debris flows, and wildfire; Bisson et al., 1987;Keller & Swanson, 1979;Wohl et al., 2012). Once in channel, LW provides many benefits to riverine ecological communities, enhancing the quantity and quality of in-stream habitats and physical (i.e., morphological and hydraulic) diversity of river systems (Collins & Montgomery, 2002;Gurnell et al., 2002;Maser & Sedell, 1994). LW can affect channel form and morphological processes by increasing or decreasing bank stability (Montgomery et al., 2003) or influencing the development of bars in braided rivers (Bertoldi et al., 2013;Mao et al., 2020). Marston (1982) reported that the amount of sediment retained by