“…Similarly, CH 4 emission levels from outlets downstream and inflow rivers upstream of reservoirs were distinct from those of the reservoir water 7,17,18 , due to variability in hydrological variables, such as water velocity and depth 2 , and dam operation strategy 19 . Temporal variability in CH 4 emissions has been attributed to changes in temperature, water column mixing, dissolved oxygen (DO) concentration, and other environmental variables, including retention time and benthic metabolism 2,20,21 . For example, CH 4 emissions were greater in summer than in other seasons at the Three Gorges Reservoir and were regulated by temperature, DO, and water velocity 2 , whereas they were only regulated by temperature at three lakes (Följesjön, Erssjön, and Skottenesjön) in southwest Sweden 20 .…”