Hydroclimate and landscape diversity drive highly variable greenhouse gas emissions from tropical and subtropical inland waters
Duvert, Clément, Borges, Alberto V., Calamita, Elisa, Rocher-Ros, Gerard, Linkhorst, Annika, Rosentreter, Judith A., Liu, Shaoda, Taillardat, Pierre, Attermeyer, Katrin, DelSontro, Tonya, Deirmendjian, Loris, Dixon, Alicia A., Grasset, Charlotte, Herreid, Allison M., Jeffrey, Luke C., Marcon, Lediane, Mwanake, Ricky M., Paranaíba, José R., Ran, Lishan, Rexroade, Adam T., Solano, Vanessa, Ulloa-Cedamanos, Francesco, Wang, Jilong, Whitmore, Keridwen M., Zhang, Liwei, López-Lloreda, Carla, Macedo, Marcia N., Oviedo-Vargas, Diana, Riveros-Iregui, Diego A., and Marzolf, Nicholas S. (2025) Hydroclimate and landscape diversity drive highly variable greenhouse gas emissions from tropical and subtropical inland waters. Nature Water, 3 (11). pp. 1303-1317.
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Abstract
(Sub)tropical inland waters are important greenhouse gas (GHG) sources, yet limited observations have long hindered broad analyses of GHG variability across this diverse region. Here, through a meta-analysis, we have examined the rates and drivers of GHG emissions from flowing and standing (sub)tropical inland waters. We find considerable spatial variation in fluxes, largely related to differences in hydroclimate, geomorphology, land cover and human disturbance. Flowing waters emit more carbon dioxide (3,387<inf>2,121</inf><sup>5,702</sup> TgCO<inf>2</inf> yr<sup>−1</sup>, expressing median<inf>first quartile</inf><sup>third quartile</sup>), methane (10.6<inf>0.1</inf><sup>28.8</sup> TgCH<inf>4</inf> yr<sup>−1</sup>) and nitrous oxide (0.62<inf>0.35</inf><sup>1.10</sup> TgN<inf>2</inf>O yr<sup>−1</sup>) than standing waters (114<inf>73</inf><sup>219</sup> TgCO<inf>2</inf> yr<sup>−1</sup>, 5.4<inf>2.1</inf><sup>9.1</sup> TgCH<inf>4</inf> yr<sup>−1</sup> and 0.03<inf>0.02</inf><sup>0.05</sup> TgN<inf>2</inf>O yr<sup>−1</sup>, respectively). (Sub)tropical inland waters release 4,238<inf>2473</inf><sup>7375</sup> TgCO<inf>2</inf>-equivalents annually, with first- to third-order streams contributing 75% of riverine emissions and lakes larger than 100 km<sup>2</sup> contributing 59% of standing water emissions. Our results suggest emissions from (sub)tropical waters are 29–72% lower than earlier estimates, a downward revision with important implications for global GHG budgets.
| Item ID: | 89947 |
|---|---|
| Item Type: | Article (Research - C1) |
| ISSN: | 2731-6084 |
| Copyright Information: | © The Author(s), under exclusive licence to Springer Nature Limited 2025. |
| Funders: | Australian Research Council (ARC) |
| Projects and Grants: | ARC DE220100852 |
| Date Deposited: | 31 Jul 2026 00:48 |
| FoR Codes: | 37 EARTH SCIENCES > 3707 Hydrology > 370702 Ecohydrology @ 50% 37 EARTH SCIENCES > 3701 Atmospheric sciences > 370104 Atmospheric composition, chemistry and processes @ 50% |
| SEO Codes: | 18 ENVIRONMENTAL MANAGEMENT > 1801 Air quality, atmosphere and weather > 180103 Atmospheric processes and dynamics @ 100% |
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