“…Such extreme non‐uniform nature of process–form interactions has enabled the river system to dissipate the fluvial energy at different scales. The previous studies on the Brahmaputra river have focused on flow–sediment variability (Fischer et al, 2017; Goswami, 1985; Karmaker & Dutta, 2015), morphological dynamics, and ecological responses through numerical modelling (Biswas et al, 2016; Karmaker & Dutta, 2016; Surabuddin Mondal et al, 2013), field investigations (Gul et al, 2018; Karmaker & Dutta, 2013), laboratory experiments (Chembolu & Dutta, 2018; Khan et al, 2021) and geo‐spatial techniques (Akhtar et al, 2011; Dubey et al, 2014; Sarma, 2005). The synthesis of these literatures has established the energy expenditure can be targeted towards a single (or multiple) fluvial processes.…”