“…We speculate that this might be due to the functional relationship, as established in laboratory experiments, is primarily relevant to bedload transport (Benavides et al., 2022; Benavides et al., 2023; Liu et al., 2019). However, in field observations, the suspended load transport cannot be disregarded (Sanford et al., 1991; Tang et al., 2023; Wang et al., 2013; Y. Li et al., 2021), especially in estuarine and nearshore areas where suspended sediment concentration and average flow velocity are relatively high, with the average maximum flow velocity at the bottom reaching 0.63 m/s and the maximum SSC reaching 988.19 mg/L (Table S1 in Supporting Information ). Therefore, it is essential to adopt alternative methods that leverage the turbulent intermittency index obtained from field data to accurately determine the critical value.…”