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ice cover
ice cover is decreasing
lakes are freezing later and breaking up earlier
less ice - more solar warming - longer growing season
lake temperature
lakes are warming
most lakes show increasing surface water temperatures
stratification
stratification lasts longer
earlier onset and later breakdown of thermal stratification
leads to less frequent mixing
longer stratification causes…
reduced oxygen replenishment
bottom waters become hypoxic or anoxic
phosphorus loading
internal phosphorus loading increases
anoxic sediments release phosphorus
fuels algal blooms
eutrophication can increase without more external nutrients
productivity
generally increases - but not everywhere
many lakes show higher productivity and more blooms
some deep lakes (L. Tanganyika) show decreased productivity due to reduced nutrient mixing