“…The joint probability distribution of particle hop distance and travel time encapsulates the relationship between granular sediment motion and topographic change (Ancey, 2010; Furbish et al., 2012; Nakagawa & Tsujimoto, 1976; Pelosi & Parker, 2014; Tsujimoto, 1978). Considerable attention has been devoted to the problem of discerning the forms of the associated marginal distributions and predicting their parameters or moments under steady, uniform macroscopic flow conditions (Abbott & Francis, 1977; Fathel et al., 2015; Furbish, Fathel, & Schmeeckle 2016; Hosseini Sadabadi et al., 2019; Lajeunesse et al., 2010; Liu et al., 2019). This objective represents an important step toward the development of models for large‐scale fluvial morphodynamics that are consistent with the physics of grain‐scale sediment transport.…”