Global Biogeochemical Cycles · 2004 · 1.3K citations · 51 references
Natural SciencesEarth SciencesEnvironmental SciencesClimate ScienceFreshwater EcologyTerrestrial EcologyCarbon CycleGreenhouse EffectGreenhouse Gas AccountingLake EcologyGreenhouse Effect ModelingMethaneMethane Emission InventoriesMethane Emission ModelingMethane EmissionsMethane Emissions InventoriesMethane FluxesTotal Phosphorus
Lake sediments are major methane sources, yet regional and global lake methane emissions remain poorly quantified. The study aimed to predict lake methane emissions using easily measured characteristics from 11 North American, 13 Swedish, and 49 literature lakes. They derived predictive equations linking lake area, depth, total phosphorus, dissolved organic carbon, methane, and anoxic volume to emissions, then applied them to estimate regional fluxes in Sweden and the U.S. upper Midwest.
Lake sediments are “hot spots” of methane production in the landscape. However, regional and global lake methane emissions, contributing to the greenhouse effect, are poorly known. We developed predictions of methane emissions from easily measured lake characteristics based on measurements for 11 North American and 13 Swedish lakes, and literature values from 49 lakes. Results suggest that open water methane emission can be predicted from variables such as lake area, water depth, concentrations of total phosphorus, dissolved organic carbon, and methane, and the anoxic lake volume fraction. Using these relations, we provide regional estimates from lakes in Sweden and the upper midwest of the United States. Considering both open water and plant‐mediated fluxes, we estimate global emissions as 8–48 Tg CH 4 yr −1 (6–16% of total natural methane emissions and greater than oceanic emission), indicating that lakes should be included as a significant source in global methane budgets.
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Biogeochemical aspects of atmospheric methane
Ralph J. Cicerone, Ronald S. Oremland · Global Biogeochemical Cycles · 1988 · 1.6K citations · Full text