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Seasonal variability of tropical wetland CH4 emissions: the role of the methanogen-available carbon pool
[摘要] We develop a dynamic methanogen-available carbon model (DMCM) to quantifythe role of the methanogen-available carbon pool in determining the spatialand temporal variability of tropical wetland CH4 emissions over seasonaltimescales. We fit DMCM parameters to satellite observations of CH4 columns from SCIAMACHY CH4 and equivalent water height (EWH) from GRACE. Over the AmazonRiver basin we found substantial seasonal variability of this carbon pool(coefficient of variation = 28 ± 22%) and a rapid decay constant(φ = 0.017 day−1), in agreement with available laboratory measurements, suggesting that plant litter is likely the prominent methanogen carbon source over this region.Using the DMCM we derived global CH4 emissions for 2003–2009,and determined the resulting seasonal variability of atmospheric CH4on a global scale using the GEOS-Chem atmospheric chemistry and transport model.First, we estimated that tropical emissions amounted to 111.1 Tg CH4 yr−1,of which 24% was emitted from Amazon wetlands. We estimated that annual tropical wetlandemissions increased by 3.4 Tg CH4 yr−1 between 2003 and 2009.Second, we found that the model was able to reproduce the observed seasonallag of CH4 concentrations peaking 1–3 months before peak EWH values.We also found that our estimates of CH4 emissions substantially improved thecomparison between the model and observed CH4 surface concentrations (r = 0.9).We anticipate that these new insights from the DMCM represent a fundamental step inparameterising tropical wetland CH4 emissions and quantifying the seasonalvariability and future trends of tropical CH4 emissions.
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[效力级别]  [学科分类] 地球化学与岩石
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