“…Consequently, suspended sediment concentrations show a high degree of scatter and sediment-rating curves can substantially underestimate or overestimate the concentrations (Horowitz, 2003). Various methods, such as subdividing the suspended sediment dataset seasonally (e.g., Walling and Webb, 1983;Mossa, 1988Mossa, , 1996Batalla and Sala, 1994), as a function of the hydrological flow conditions (e.g., Asselman, 2000;Hudson, 2003) or choosing a threshold discharge (e.g., Serrat, 1999) have been developed to improve the C-Q relationships. In this study, the primary dataset was divided into samples collected during low flows (≤3.5 m 3 s − 1 ) and those taken during flood events (N3.5 m 3 s − 1 ) and different relations were constructed for each case.…”