Isotopic signatures of methane emissions from tropical fires, agriculture and wetlands: the MOYA and ZWAMPS flights

dc.contributor.authorEuan G. Nisbet
dc.contributor.authorGrant Allen
dc.contributor.authorRebecca Fisher
dc.contributor.authorJames L. France
dc.contributor.authorJames Lee
dc.contributor.authorDavid Lowry
dc.contributor.authorMarcos Andrade
dc.contributor.authorThomas J. Bannan
dc.contributor.authorPatrick Barker
dc.contributor.authorPrudence Bateson
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T14:18:35Z
dc.date.available2026-03-22T14:18:35Z
dc.date.issued2021
dc.descriptionCitaciones: 16
dc.description.abstractWe report methane isotopologue data from aircraft and ground measurements in Africa and South America. Aircraft campaigns sampled strong methane fluxes over tropical papyrus wetlands in the Nile, Congo and Zambezi basins, herbaceous wetlands in Bolivian southern Amazonia, and over fires in African woodland, cropland and savannah grassland. Measured methane <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> isotopic signatures were in the range -55 to -49‰ for emissions from equatorial Nile wetlands and agricultural areas, but widely -60 ± 1‰ from Upper Congo and Zambezi wetlands. Very similar <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> signatures were measured over the Amazonian wetlands of NE Bolivia (around -59‰) and the overall <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> signature from outer tropical wetlands in the southern Upper Congo and Upper Amazon drainage plotted together was -59 ± 2‰. These results were more negative than expected. For African cattle, <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> values were around -60 to -50‰. Isotopic ratios in methane emitted by tropical fires depended on the C3 : C4 ratio of the biomass fuel. In smoke from tropical C3 dry forest fires in Senegal, <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> values were around -28‰. By contrast, African C4 tropical grass fire <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> values were -16 to -12‰. Methane from urban landfills in Zambia and Zimbabwe, which have frequent waste fires, had <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> around -37 to -36‰. These new isotopic values help improve isotopic constraints on global methane budget models because atmospheric <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> values predicted by global atmospheric models are highly sensitive to the <i>δ</i><sup>13</sup>C<sub>CH<sub>4</sub></sub> isotopic signatures applied to tropical wetland emissions. Field and aircraft campaigns also observed widespread regional smoke pollution over Africa, in both the wet and dry seasons, and large urban pollution plumes. The work highlights the need to understand tropical greenhouse gas emissions in order to meet the goals of the UNFCCC Paris Agreement, and to help reduce air pollution over wide regions of Africa. This article is part of a discussion meeting issue 'Rising methane: is warming feeding warming? (part 2)'.
dc.identifier.doi10.1098/rsta.2021.0112
dc.identifier.urihttps://doi.org/10.1098/rsta.2021.0112
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/45761
dc.language.isoen
dc.publisherRoyal Society
dc.relation.ispartofPhilosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences
dc.sourceRoyal Holloway University of London
dc.subjectWetland
dc.subjectEnvironmental science
dc.subjectMethane
dc.subjectAmazon rainforest
dc.subjectTropics
dc.subjectTropical savanna climate
dc.subjectIsotopic signature
dc.subjectDry season
dc.subjectHydrology (agriculture)
dc.titleIsotopic signatures of methane emissions from tropical fires, agriculture and wetlands: the MOYA and ZWAMPS flights
dc.typearticle

Files