Climate Change

Lake thermal dynamics have been altered around the world as a result of climate change, necessitating a predictive understanding of how climate will continue to alter lakes in the future as well as the associated uncertainty in these predictions. We found that the dominant source of uncertainty varied among the thermal metrics, as thermal metrics associated with the surface waters (surface water temperature, total ice duration) were driven primarily by climate model selection uncertainty, while metrics associated with deeper depths (bottom water temperature, stratification duration) were dominated by lake model selection uncertainty.

Five lake models forced by four different climate model projections are used to simulate historic and future change in lake evaporation for Lake Kinneret (Israel). There were considerable differences in simulated evaporation rates among the models, with the annual average evaporation rates varying between 1232 mm year-1 and 2608 mm year-1 during the historic period (1901-2005). By the end of the 21st century (2070-2099), annual average evaporation rates would increase by 9-22% under RCPs 2.6-8.5. Our projections suggest that the water balance of Lake Kinneret could experience a deficit of 14-40% this century.

Undergraduate and graduate students who completed the module showed increased familiarity with ecological forecasts and forecast uncertainty. Integrating ecological forecasting into undergraduate ecology curricula will enhance students’ abilities to engage and understand complex ecological concepts.

Methane is typically produced in lake sediments, with the rate of methane production being strongly temperature dependent. Future warming of bottom waters will likely result in an increase in methane production rates of 13%–40% by the end of the century, with many low-latitude lakes experiencing an increase of up to 17 times the historical (1970–1999) global average under RCP 8.5.

Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 ± 7.0 days earlier and end 11.3 ± 4.7 days later by the end of this century. It is very likely that this 33.3 ± 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.