Warm on top, cold below: unexpected greenhouse gas effect in lakes
A research team led by the University of Basel and the Université de Montréal examined how the ongoing climate warming affects the “behavior” of lakes. The researchers found out why, in near-bottom waters, lakes may even cool down despite warming at the surface, and what the consequences are for the production and emission of greenhouse gases. The results of the study were published in the most recent edition of the journal Limnology and Oceanography Letters.
Lakes play an important role in the global carbon cycle, acting as large natural bioreactors. The temperature of a lake represents an important constraint on the amount of carbon dioxide and methane it emits into the atmosphere. It was generally assumed that global warming stimulates microbial respiratory processes and the production of these greenhouse gases, while at the same time reducing the carbon storage in lake sediments. An international research team has now examined these interactions more closely and discovered unexpected effects.
The research project not only targeted the direct effects of global warming, but also the indirect ones. The main focus of the investigations was the water temperature and greenhouse gas production in the deeper parts of the lakes. “We don’t want to question the fundamentals of thermodynamics. There is no doubt that the rates of respiratory metabolic processes in lakes are generally higher at increased water temperatures,” explains Professor Moritz Lehmann from the Department of Environmental Sciences at the University of Basel. “However, climate change will not cause every lake to warm up everywhere.”
Warming near the surface, cooling near the bottom
Lakes worldwide are warming at the surface. However, they are also losing transparency due to increased algae production and enhanced turbidity of the lake water. “The surface-water warming and the loss of transparency have the effect that more heat is trapped in the upper layers of the lakes, leaving the deeper waters thermally isolated,” says lead author Dr. Maciej Bartosiewicz from the Department of Environmental Sciences at the University of Basel. “Under some circumstances, this can even lead to the cooling of water masses near the bottom of the lake.”
The subtle cooling slows down respiratory decay processes and carbon dioxide production in the lakes, increasing carbon burial within the sediments. Model simulations suggest that the observed effects are most pertinent to relatively small and shallow lakes, which make up approximately half of the global lake surface.
Less carbon dioxide, more methane
The increased differential warming in lakes has yet another effect: the pronounced thermal stratification entails that the deeper water layers do barely mix and are poorly ventilated, which can lead to prolonged anoxia. Under these oxygen-free conditions, methane production by anaerobic microorganisms is enhanced.