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. 2022 Jun 24;8(25):eabi8716. doi: 10.1126/sciadv.abi8716

Table 1. Downward reevaluation of tropical lacustrine CO2, CH4, and N2O emissions.

Air-water flux of CO2 (FCO2), CH4 (FCH4, diffusive and ebullitive), and N2O (FN2O) integrated for African tropical and pan-tropical lakes (with a surface area >0.1 km2) compared to previous estimates (details in table S4) (1, 3, 4, 9, 31, 47). Values with a single asterisk (*) correspond to the scaling using the original HydroLAKES surface area (29), including an unrealistic surface area value of 18,752 km2 for Lake Chad. Values with a double asterisk (**) were obtained with a more recent surface area value of 2603 km2 for Lake Chad (30). n.a., not available.

FCO2 Diffusive FCH4 Ebullitive FCH4 FN2O
TgC year–1 TgCH4 year–1 TgCH4 year–1 GgN2O-N year–1
African tropical lakes
This study (*) 6.3 ± 1.9 1.3 ± 0.3 2.3 (0.8–5.5) 0.3 ± 0.2
This study (**) 3.3 ± 1.0 0.4 ± 0.1 1.8 (0.6–4.1) −0.1 ± 0.1
Previous studies 35.6 n.a. n.a. 3.7
Pan-tropical lakes
This study (*) 20.5 ± 10.7 1.6 ± 0.4 4.9 (1.7–11.4) 0.8 ± 1.1
This study (**) 17.5 ± 9.5 0.7 ± 0.2 4.4 (1.5–10.0) 0.4 ± 0.7
Previous studies 103.1 to 441.6 3.1 22.2 6.5