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Regional Variability and Drivers of Below Ice CO2 in Boreal and Subarctic Lakes
Authors:Blaize A. Denfeld  Pirkko Kortelainen  Miitta Rantakari  Sebastian Sobek  Gesa A. Weyhenmeyer
Affiliation:1.Department of Ecology and Genetics/Limnology, Evolutionary Biology Center,Uppsala University,Uppsala,Sweden;2.Finnish Environment Institute,Helsinki,Finland;3.Department of Environmental Sciences,University of Helsinki,Helsinki,Finland;4.Department of Physics,University of Helsinki,Helsinki,Finland
Abstract:Northern lakes are ice-covered for considerable portions of the year, where carbon dioxide (CO2) can accumulate below ice, subsequently leading to high CO2 emissions at ice-melt. Current knowledge on the regional control and variability of below ice partial pressure of carbon dioxide (pCO2) is lacking, creating a gap in our understanding of how ice cover dynamics affect the CO2 accumulation below ice and therefore CO2 emissions from inland waters during the ice-melt period. To narrow this gap, we identified the drivers of below ice pCO2 variation across 506 Swedish and Finnish lakes using water chemistry, lake morphometry, catchment characteristics, lake position, and climate variables. We found that lake depth and trophic status were the most important variables explaining variations in below ice pCO2 across the 506 lakes. Together, lake morphometry and water chemistry explained 53% of the site-to-site variation in below ice pCO2. Regional climate (including ice cover duration) and latitude only explained 7% of the variation in below ice pCO2. Thus, our results suggest that on a regional scale a shortening of the ice cover period on lakes may not directly affect the accumulation of CO2 below ice but rather indirectly through increased mobility of nutrients and carbon loading to lakes. Thus, given that climate-induced changes are most evident in northern ecosystems, adequately predicting the consequences of a changing climate on future CO2 emission estimates from northern lakes involves monitoring changes not only to ice cover but also to changes in the trophic status of lakes.
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