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Generalized Additive Models of Climatic and Metabolic Controls of Subannual Variation in pCO 2 in Productive Hardwater Lakes
Author(s) -
Wiik E.,
Haig H. A.,
Hayes N. M.,
Finlay K.,
Simpson G. L.,
Vogt R. J.,
Leavitt P. R.
Publication year - 2018
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1029/2018jg004506
Subject(s) - environmental science , diel vertical migration , photosynthesis , carbon cycle , carbon dioxide , atmospheric sciences , respiration , climate change , flux (metallurgy) , climatic variability , ecology , ecosystem , environmental chemistry , chemistry , biology , geology , botany , organic chemistry
Abstract Spatiotemporal variation in climate and weather, allochthonous carbon loads, and autochthonous factors such as lake metabolism (photosynthesis and respiration) interacts to regulate atmospheric CO 2 exchange of lakes. Understanding this interplay in diverse basin types at different timescales is required to adequately place lakes into the global carbon cycle and predict CO 2 flux through space and time. We analyzed 18 years of data from seven moderately hard lakes in an agricultural prairie landscape in central Canada. We applied generalized additive models and sensitivity analyses to evaluate the roles of metabolic and climatic drivers in regulating CO 2 flux at the intra‐annual scale. At mean conditions with respect to other predictors, metabolic controls resulted in uptake of atmospheric CO 2 when surface waters exhibited moderate primary production but released CO 2 only when primary production was very low (<8 μg/L or when dissolved nitrogen was elevated (>2,000 μg/L), implying that respiratory controls offset photosynthetic CO 2 uptake under these conditions. Climatically, dry conditions increased the likelihood of in‐gassing, likely due to evaporative concentration of base cations and/or reduced allochthonous carbon loads. While more research is required to establish the relative importance of climate and metabolism at other timescales (diel, autumn/winter), we conclude that these hard fresh waters characteristic of continental interiors are mainly affected by metabolic drivers of pCO 2 at daily‐monthly timescales, are climatically controlled at interannual intervals, and are more likely to in‐gas CO 2 for a given level of algal abundance than are soft water, boreal ecosystems.