Synergistic Effects of Warming and Internal Nutrient Loading Interfere with the Long-Term Stability of Lake Restoration and Induce Sudden Re-eutrophication.

For DO, simulated results pointed to a decreasing trend since 1980 ( Figure S8 ) with rates of −0.011 and −0.023 mg·L –1 ·a –1 in the epi- and hypolimnion, respectively, and −0.021 mg·L –1 ·a –1 for the whole lake (Mann–Kendall test, p < 0.001).

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