“…Commonly, a paucity of high-frequency and long-term SSC or other proxy data (e.g., turbidity) necessitate the assumption that suspended sediment yield per unit discharge is static (Gray et al, 2003;Jones, Stevens, Horsburgh, & Mesner, 2011). However, as these records continue to grow and more frequent measurements become possible with advanced technologies (Gray & Gartner, 2009;Rai & Kumar, 2015), there is a growing body of evidence that the yield of suspended sediment per unit discharge varies over a wide range of time scales, from individual storms (Bača, 2008;Gellis, 2013) to interannual timeframes (Herndon et al, 2015;Rodríguez-Blanco, Taboada-Castro, & Taboada-Castro, 2010;Warrick, 2015). These changes manifest as variations in the rating curve over time.…”