“…Freshwater inflow therefore directly influences residence time and nutrient loading (Howarth & Marino, 2006; Wolanski & Elliott, 2015), which in turn regulates primary production dynamics (Anandraj, Perissinotto, & Nozais, 2007; Eyre, 1998; Howarth & Marino, 2006). A decrease in magnitude of riverine flows may result in lengthened flushing times, decreased magnitude of riverine flows and dilution of nutrient concentrations (De Villiers & Thiart, 2007) and increased mouth closure (Allanson & Winter, 1999; Schumann et al, 1999; Wolanski & Elliott, 2015), thereby influencing the rate at which the process of eutrophication occurs (Ferreira et al, 2011; Lemley, Adams, Taljaard, & Strydom, 2015). For instance, the addition of wastewater flows to two South African TOCEs resulted in eutrophic levels of chlorophyll‐a (Thomas, Perissinotto, & Kibirige, 2005).…”