“…Higher temperature increases the release of nitrogen from soil, and lower stream flows decrease the dilution capacity of rivers (Whitehead et al, 2006). However, the impact on eutrophication is not straightforward due to the complex interaction between nutrient, light, temperature, residence time and flow conditions (Jeppesen et al, 2005;Yang and Flower, 2012). Increased surface water temperature can indirectly lead to stronger stratification and regeneration of water column nutrients, which can intensify eutrophication (Rabalais et al, 2009).…”